Next Article in Journal
Automated and Quantitative Mineralogy Applied to Chromite Ore Characterization and Beneficiation
Next Article in Special Issue
Campiglia Marittima Skarn (Tuscany): A Challenging Example for the Evolution of Skarn-Forming Models
Previous Article in Journal
Coal-Based Activated Carbon via Microwave-Assisted ZnCl2 Activation for Methyl Violet 2B Dye Removal: Optimization, Desirability Function, and Adsorption Mechanism
 
 
Search for Articles:
Title / Keyword
Author / Affiliation / Email
Journal
Article Type
 
 
Advanced Search
 
Section
Special Issue
Volume
Issue
Number
Page
 
Journals
Minerals
Volume 13
Issue 3
10.3390/min13030439
minerals-logo
Submit to this Journal Review for this Journal Propose a Special Issue
► Article Menu

Article Menu

share Share announcement Help format_quote Cite question_answer Discuss in SciProfiles thumb_up
...
Endorse textsms
...
Comment
first_page
settings
Order Article Reprints
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Review

Review of Polymetallic Mineralization in the Sila and Serre Massifs (Calabria, Southern Italy)

by
Rosa Anna Fregola
1,*,
Antonio Ciccolella
1,
Vincenzo Festa
1,
Giovanni Ruggieri
2,
Emanuela Schingaro
1,
Fabrizio Tursi
3 and
Gennaro Ventruti
1
1
Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari Aldo Moro, Via Orabona 4, 70125 Bari, Italy
2
Istituto di Geoscienze e Georisorse (IGG), Consiglio Nazionale delle Ricerche (CNR), Via La Pira 4, 50121 Firenze, Italy
3
Dipartimento di Scienze della Terra, Università degli Studi di Torino, Via Valperga Caluso 35, 10125 Torino, Italy
*
Author to whom correspondence should be addressed.
Minerals 2023, 13(3), 439; https://doi.org/10.3390/min13030439
Submission received: 28 February 2023 / Revised: 16 March 2023 / Accepted: 17 March 2023 / Published: 19 March 2023
(This article belongs to the Special Issue Understanding the Geologic History of Italy: Perspectives from Geochemistry, Geology and Mineralization)
Browse Figures
Review Reports Versions Notes

Abstract

:
We provide an updated overview of the known mineral deposits from the Sila and Serre Massifs in Calabria, contributing to setting their genesis within a complex geologic history, starting from the late-Carboniferous. We summarize the mineralization reported in the literature, with a critical review of the host tectonic units, by taking into account the upgrades in the knowledge of these areas. We also set them in updated geological maps and in stratigraphic columns, highlighting the crustal levels to which they pertain. Despite the geologic and minerogenetic similarities potentially existing with late- to post-Variscan mineral deposits from other regions (e.g., Sardinia and French Central Massif), the scientific literature on the Calabria mineralization is out-of-date and not exhaustive. Moreover, these ore deposits were likely considered not economically attractive enough to stimulate new scientific studies. However, in our opinion, such studies are needed to resolve the main open questions, which rely on deciphering the origin and age of mineralization. Finally, research for critical elements hosted by the Sila and Serre mineralization (e.g., In, Ge and Ga in sphalerites) is a possible interesting new perspective.

1. Introduction

The study of mineralization from metal-carrying fluids during orogenic events is essential to assess the budget and availability of elements in their life cycle, from the deep Earth’s lithosphere to the atmosphere, biosphere and hydrosphere (e.g., [1]). Hence, it is important to outline the different types of mineralization developed during poly-orogenic events into the tectonic, metamorphic, magmatic and sedimentary evolution of a geologic area, in order to relate deep Earth volatiles and metal factories into the different geodynamic settings.
Our paper aims to provide an updated and extensive overview of the scientific literature on mineral deposits in the Sila and Serre Massifs from Calabria (southern Italy). Calabria has been a crucial district for raw metals exploitation starting from the Bronze and Iron ages. Recent historical and archaeological literature on the Calabria ores and mines (e.g., [2,3]) is wider than the scientific one. Particularly, focus on the iron mining industry, once active in the Stilaro valley of the Serre area, is found in the Italian archeo-minerary literature [4,5,6].
The mineralizations in Calabria have been described throughout time, for both industrial exploitation and geological interest. In particular, the first reports came between the first half of the 19th century and the 1940’s [7,8,9,10,11,12,13,14,15,16,17,18,19,20,21,22,23,24,25,26,27,28,29,30]. In order to ascertain the mining potential of Calabria, and to determine the relationships between host rocks and mineralization, a field geological survey was started in 1946 by “Centro Ricerche Geominerarie” of the Italian Institute for Industrial Reconstruction [31], and by “Centro Studi Silani” of the Italian C.N.R. [32]. At the beginning, the study was restricted to a few localities of the Sila [33,34,35,36,37] and Serre Massifs [38]. After that, some prospecting campaigns were performed by the Italian “Comitato Nazionale per l’Energia Nucleare” [39,40,41,42,43,44]. In 1974, the Italian Government recommended a regional geochemical survey as a key tool for a mineral potential assessment program in Calabria. This program was performed by a mining research company (RIMIN Spa), by the Italian “Ministero dell’Industria, Commercio e Artigianato” (MICA), and by “Ente Nazionale Idrocarburi” (ENI); geochemical analyses were conducted on thousands of samples collected from different localities throughout Calabria [45,46,47,48,49,50]. The analyses revealed positive anomalies of Pb, Zn, Mo, As, W, Ba, Sn, Ag and Au, for the Rossano-Longobucco-Savelli areas (Sila); As, Be, Ba, Pb and Zn, to the north of Catanzaro (Sila); Hg and As, to the south of the Savuto river (Sila); and Pb, As, Zn and Mo, in the western part of the Stilo area (Serre). Results from samples collected during the geochemical surveys of the 1970′s and 1980′s were subsequently used to compile a geochemical baseline map illustrating the regional variability of twelve selected elements: Cu, Pb, Zn, Hg, Fe, Mn, Ba, As, W, Mo, Sn and Be [51].
Early efforts to survey the known scientific literature on mineralization from the Sila and Serre Massifs were made, trying to infer some hypotheses on the ore genesis. These hypotheses were generally based on lithostratigraphic considerations rather than on analytical results (e.g., [52,53,54,55,56]).
We provide a critical review of the literature on the polymetallic mineralizations in the Sila and Serre Massifs, with emphasis on the still-open issue of the ore genesis, and we build up a dataset that paves the way to future research on the subject. This dataset reviews the lithostratigraphic approach of the most relevant background literature on this topic (e.g., [53,54,55,57]) by trying to solve the emerging inconsistencies with respect to the present geologic knowledge on the poly-orogenic evolution of the Calabria’s crystalline basement. The main areas of mining interest in the middle-eastern sectors of Calabria that will be considered (Figure 1) are: (i) Longobucco-Corigliano-Rossano, San Giovanni in Fiore-Savelli-Cerenzia, Catanzaro-Tiriolo-Gimigliano (in the Sila territory); and (ii) Stilo-Pazzano-Bivongi, San Todaro-Calatria-Caulonia (in the Serre area). A comprehensive account on ore geology will be presented following an overview of the geological context, and a general description of mineralization framed into the host tectonic units recognized in the literature.

2. Geological Setting

The Calabria-Peloritani terrane [58], i.e., the “calabro-peloritano arc” [59], is a nappe pile stacked-up during the Alpine orogeny. Amodio-Morelli et al. [59] suggested the distinction of several Alpine tectonic units, which in the Sila and Serre Massifs of Calabria (Figure 2 and Figure 3) are: the Gimigliano Unit, the Diamante-Terranova Unit, the Bagni-Fondachelli Unit, i.e., the Fiume Pomo Unit [60], the Polia-Copanello Unit, the Monte Gariglione Unit, the Longobucco-Longi-Taormina Unit, and the Stilo Unit.
The complex of ophiolite tectonic units (Gimigliano and Diamante-Terranova units) affected by high pressure–low temperature (HP-LT) metamorphism (e.g., [61]) underlies the Fiume Pomo Unit, which, in turn, lies below the Castagna Unit (e.g., [62,63,64]).
The Fiume Pomo Unit is characterized by phyllites equilibrated during the Variscan orogeny under greenschist facies conditions [65]. The Castagna Unit is dominated by orthogneisses (mostly augen gneisses), minor muscovite-leucocratic gneisses, paragneisses, actinolite schists, and amphibolites, that equilibrated under amphibolite facies conditions during the Variscan orogeny [65,66]. Later, these two units were locally affected by the Alpine tectono-metamorphic overprint, especially along ductile shear zones [65,66,67].
Some authors [68,69,70] concluded that the metamorphic and intrusive successions within the Polia-Copanello, Monte Gariglione, Longobucco-Longi-Taormina, and Stilo units belong to a nearly continuous late Variscan continental crust block. Accordingly, Festa et al. [71] proposed a simplified tectonic scheme with this continental crust block belonging to a single large Alpine nappe, i.e., the Sila-Serre Unit (Figure 2, Figure 3 and Figure 4); this nappe overthrusted the complex of ophiolite units and the Fiume Pomo and Castagna ones (e.g., [66,72], and references therein).
The almost complete late Variscan continental crustal block shows a thickness up to about 23 km [69,70,77,78,79], consisting of three crustal levels: lower, middle, and upper (Figure 2b). The lower crust (formerly assigned to the Monte Gariglione and Polia-Copanello units) shows a thickness of about 7–8 km, and is composed of mafic and felsic granulites, below, and of amphibolite-granulite facies migmatitic paragneisses, above (e.g., [70,80,81,82]), juxtaposed by a shear zone [83].
The late Variscan crustal block continues upwards with the up to about 12 km thick Sila and Serre batholiths [84,85] that occupy the middle crust (Figure 2, Figure 3 and Figure 4) [70,77,78]. The main magma affinity of the batholiths is calc-alkaline with isotopic signatures, indicating mantle-crust mixed origin [85,86,87,88].
The Sila and Serre batholiths mostly consist of late Carboniferous-early Permian tonalites, quartz-diorites, and two-mica peraluminous granites, biotite granodiorites and occasional small bodies of gabbro-diorite (Figure 2, Figure 3 and Figure 4); sporadic volumes of aplite-pegmatite dikes are present especially along the roof of the batholiths [84,85,89,90,91], and within the related upper crust host rock (e.g., [92,93]). A wide migmatitic border zone is observed in-between batholiths and lower crustal migmatitic paragneisses; in the Sila Massif, the contact is characterized by an amphibolite-granulite facies shear zone, with supra- to sub-solidus deformation conditions [73,94,95]. The contact between granitoids and the upper crustal host rock is sharp and marked by an extensive metamorphic aureole (Figure 2, Figure 3 and Figure 4) [92,93,96,97,98].
The upper crust consists of Variscan tectono-metamorphic units composed of amphibolite facies metapelites and meta-greywackes (i.e., Mandatoriccio and Mammola units), and a succession of phyllites, meta-carbonates, and acidic to mafic metavolcanites metamorphosed under sub-greenschist to greenschist facies conditions (i.e., Bocchigliero and Stilo-Pazzano units) [74,96,97,98,99]. It is worthy to underline that these Variscan tectono-metamorphic units, together with Sila and Serre batholiths, were formerly ascribed to the Longobucco-Longi-Taormina and Stilo units [59].
Magmatic products, consisting of porphyritic, mafic and felsic dikes and sills, with rhyolitic to dacitic, and andesitic compositions, intruded the Sila and Serre batholiths, and the upper crust host rock [100,101]. This calc-alkaline to alkali-calcic affinity magmatism occurred mostly during the early Permian (between 295 and 277 Ma) crust exhumation and transtentional tectonics [100].
Finally, a Mesozoic cover, dominated by carbonate rocks, discordantly overlies the crystalline bedrock (e.g., [102,103,104]) and represents the so-called “Longobucco cover”, in the Sila Massif [75], and the “Stilo cover”, in the Serre Massif, as the upper part of the Sila-Serre Unit [71] (Figure 2, Figure 3 and Figure 4).

3. Literature Background on Polymetallic Mineralization

In this section, we report the literature background on polymetallic mineralization in the Sila and Serre Massifs, summarized in Table A1 and Table A2 following a temporal order, from pre-Alpine to post-Alpine, and listed with progressively numbered locations and short informative descriptions. The same numbered locations are indicated in the schematic geologic maps (Figure 2 and Figure 3) and cross-sections (Figure 4).
A few pioneering papers describing the mineralization in Calabria were largely based on field observations, not supported by the analytical characterization of minerals. In these papers, two kinds of approaches were adopted: (i) descriptive, focussed on an area with several mineralization sites close to each other (e.g., [36,37]); (ii) lithostratigraphic, where several mineralization sites (scattered in areas far from each other) were framed in the same host tectonic unit (e.g., [53,54,55,57]). This second approach gives a global view highlighting possible genetic links between single mineralization sites, and allows immediate identification of inconsistencies with the updated literature on orogenic events recorded in Calabria’s crystalline basement. Specifically, according to De Vivo et al. [53], every mineralization is hosted by units of continental derivation, and most of them would be genetically linked to the late-Variscan magmatic intrusions; mineralization occurrences related to sedimentary and metamorphic processes were found only in a few cases. These authors observed differences in the mineralization occurring in the Longobucco, Monte Gariglione, and Stilo units, all affected by late-Variscan magmatic intrusions. In the Longobucco Unit, polymetallic Pb-Zn-Cu-Fe-As mineralization (sphalerite, galena, pyrite, arsenopyrite, chalcopyrite, marcasite and malachite) were reported, with calcite, quartz and fluorite as gangue minerals. They were mainly found in the contact aureole developed in the phyllites of the pre-Alpine Bocchigliero Unit, especially at the top of the Sila batholith, where the effect of the contact metamorphism is more intensive. Moreover, primary uranium mineralization within granites of the Longobucco Unit was hypothesized, based on the finding of secondary autunite and torbernite deposited in the nearby lacustrine sediments. Differently, in the Monte Gariglione Unit, the usual metalliferous minerals were not found; this unit would be characterized by the presence of primary accessory minerals (monazite and zircon) containing more than 6.35% ThO2 [39,40,44,53,105]. In the Stilo Unit, Mo-mineralization (veinlets of molybdenite with quartz as gangue mineral, found in the Serre area), and Ba-mineralization (baryte found in the Sila and Serre areas), occurred within the late-Variscan granites; additionally, Pb-Zn-Fe-Ag-As-Cu mineralization (sphalerite, galena, pyrite, arsenopyrite, and chalcopyrite) were found in the granitic and metamorphic rocks adjacent to the intrusions [53].
In line with De Vivo et al. [53], Bonardi et al. [54] argued that, apart from a few recent mineralizations, mainly pre-Alpine mineralized systems occurred in Calabria; most of them were split-up during the Alpine evolution. These authors took into consideration metallic and not-metallic mineralization as well, and proposed some genetic hypotheses, by distinguishing them into: (i) pre-Alpine, stratabound and vein-type, within metamorphic and igneous rocks; (ii) Alpine, mainly stratabound, within metamorphic and sedimentary rocks; (iii) recent, of alluvial type [54]. In more details, the pre-Alpine stratabound mineralization, represented by magnetite, graphite and sulphides (i.e., pyrite, chalcopyrite, galena, sphalerite and pyrrothite), are found within the metamorphic rocks of the Bagni, Polia-Copanello and Stilo units, whereas the vein-type sulphide (arsenopyrite, pyrite, chalcopyrite, sphalerite and pyrrothite) mineralization occurs in the Stilo and Polia-Copanello units. The pre-Alpine mineralization hosted by igneous rocks consists mainly of sulphides (molybdenite, sphalerite, galena, pyrite, chalcopyrite, pyrrothite, arsenopyrite), and subordinately of baryte, fluorite and U-bearing minerals, occurring within the Longobucco, Stilo and Polia-Copanello units. It was hypothesized that the pre-Alpine mineralization within igneous rocks were connected to a Variscan porphyry copper-molybdenum system, subsequently split-up during the Alpine tectonic evolution [54]. However, all the genetic hypotheses put forward by these authors were not supported by any analytical investigation of the minerals, nor by the few fluid inclusion studies available for the Calabrian mineralization [106,107,108]. Concerning the Alpine mineralizations, they were reported within the San Donato Unit (baryte, cinnabar and galena), in the ophiolitic units derived from Jurassic-Cretaceous oceanic crust (the Gimigliano, Malvito, Diamante-Terranova units, with pyrite and chalcopyrite mainly found in the Catena Costiera territory), and within the clastic sediments of the Miocene deposits (Th, Mn, S, NaCl and lignite). Finally, the recent mineralization would be constituted by the radioactive ones of secondary origin occurring in the Longobucco area [54].
Later, Lorenzoni et al. [55] examined two possible main factors controlling the metallogenesis and distribution of mineralization in the different tectonic units: (i) different types of metamorphism; (ii) magma emplacement depth and type of magmatic differentiation. According to Colonna and Zanettin-Lorenzoni [109], the Variscan metamorphism that affected the upper crustal rocks of the Bagni Unit did not control neither the distribution nor the concentration of ore minerals such as pyrite, but this would rather reflect primary sedimentary concentrations. On the contrary, Lorenzoni et al. [55] suggested that intensive metasomatic effects and mobilization producing metal concentration (mostly iron) took place in rocks of the lower and intermediate crust, during amphibolite-granulite facies Variscan metamorphism. Concerning the subsequent Alpine metamorphism, the Bagni Unit would have been only marginally affected, with no evident modification of the mineralization that was already present at the end of the Variscan orogenesis [55]. In contrast, the Castagna Unit, consisting of the pre-Alpine gneisses intruded by granodiorites, and pertaining aplite-pegmatites, would have suffered a very intense Alpine dynamic metamorphism [55]. Here, Fe-Cu sulphides mineralization linked to aplite-pegmatites were occasionally found in the Castagna Unit, only where the primary lithotypes were preserved with respect to the Alpine tectono-metamorphic events [55]. This observation led the authors to infer that primary concentrations of ore minerals were dispersed by the subsequent Alpine metamorphism, and that the scarcity of ore mineralization in the Alpine ophiolitic units might be partly related to this effect, as in the case of the Gimigliano Unit, where only a few lenses of ore minerals were found within metabasites [55]. The spatial relationship existing between most of the Calabria ore mineralization and the late Variscan intrusions was observed by many authors (e.g., [53,55]), even though their genetic association is still to be proved. Investigating the role of intrusion depth and the degree of differentiation, it was observed that radioactive minerals were linked to the more differentiated intrusions, whereas Fe-Pb-Zn-As-Cu sulphides were related to weakly differentiated zones [55]. It was concluded that anatectic melts could not produce ore concentrations in the lower crust, whereas the late Variscan magmas with a mixed mantle-crust source promoted concentrations of polymetallic mineralization in the deeper granodiorite, and in the roof of the shallow two-micas granite and granodiorite [55].
Finally, Zanettin-Lorenzoni and Zuffardi [56] considered the Calabria-Peloritani Arc as a well-defined metallogenic province, which is characterized by some similarities with Sardinia. These authors also considered it as a barren region in the metallogenic maps of the Mediterranean area, because of the small size of its mineralization despite their numerous occurrences [56].

4. Mineralizations in the Sila Massif in an Updated Geological Framework

In this section, the scientific literature on three major areas of historical mining interest in the Sila Massif is reviewed: (i) Longobucco-Corigliano-Rossano; (ii) San Giovanni in Fiore-Savelli-Cerenzia; (iii) Catanzaro-Tiriolo-Gimigliano. Data on geochemical anomalies for specific metal elements in some localities [46,47,51,107] are detailed. Limited information from the literature on the amount of metallic minerals once extracted are also reported for some mining sites. The list of mineralization sites in the Sila Massif is shown in Table A1, where we report a summary of the available literature information and, in the last column, a review of the occurrences of mineral deposits with respect to the current tectono-magmatic and -metamorphic units. The same mineralization sites are reported on the geological map (Figure 2c) and the stratigraphic column (Figure 4a).

4.1. Longobucco-Corigliano-Rossano Area

4.1.1. Longobucco (CS) (Sites n. 6,7,8a,8b,8c,20; Table A1; Figure 2c and Figure 4a)

Several remarks about ancient mines once active in the Longobucco area are reported in the oldest literature (e.g., [7,8]), even though in more recent times traces of those mines were hardly found [37]. Argentiferous galena, bournonite and arsenopyrite characterized this area, with a higher Ag-content of galena hosted by phyllites, which form the granite country rocks in the area [7]. Longobucco was historically known especially for the extraction of silver from argentiferous galena, with an annual average production of 87 kg of Ag, from 1268 to 1277. In the first half of the 16th century, the Argentera of Longobucco was considered the most important silver mine; on 1645, the excavation of a galena dike close to the Trionto river produced just 4 parts of silver over 100 parts of galena (e.g., [3,110]). The Longobucco mineralizations were prospected and exploited between 1723 and 1783, and at the beginning of the 19th century, when Ag-Pb-Sb ± Cu-Fe were extracted [8,9,111]. From 1828 to 1832, the “Acqua di Radica” site produced 1800 “cantari” of Pb [17]. Anyway, galena was hardly found in the Longobucco area. At the end of the 19th century, the finding of some galena within landslide debris at Spartari and along the Macrocioli river was reported, but a galena ore body was not observed [23]. Indeed, foundries for the extraction of Ag from argentiferous galena were located just along the Macrocioli river [110]. For the Longobucco area, positive geochemical anomalies of Zn-Fe-Sb (neither Pb nor Ag) were detected in soils [107].
Ore bodies hosted by magmatic rocks (granite, quartz-monzonite, porphyritic and quartz-monzonitic dikes), and metamorphic rocks (schists and hosted marble lenses) were studied [31,32,34,35,37]. A lower sulphides content was reported for dikes hosted by phyllites, with respect to those within granitic rocks [37,53]. Multiple fracturing and mineralization episodes were recognized, producing the following paragenetic sequence [37]: calcite I + sphalerite; quartz + pyrite (± marcasite); calcite II; galena + chalcopyrite; (secondary) calcite III. Sphalerite is the most abundant ore mineral [53], whereas galena was sporadically found in small veins filling fractures within calcite II [37]. Noteworthy, galena mineralization was reported from quartz veins, hosted by granitic rocks close to the contact with Lias carbonate rocks. This mineralization was considered as related to post-Triassic porphyritic dikes, and of Mesozoic (post-Lias) age [29]. However, dike magmatism in the area is well constrained to the late Carboniferous–early Permian age [100]. Therefore, these carbonate rocks would be interbedded in the Variscan Bocchigliero Unit succession [99].
Numerous mineralized sites are reported in the literature for this area (Table A1; [54]). In particular, Pb-Zn ± Fe-Cu mineralization (sites n. 6, 7, 8a) of suggested hydrothermal origin were observed in veins within Variscan granitoids, close to the contact with phyllites of the Longobucco Unit [54]. In addition, pyrite vein mineralization within carbonatic lenses intercalated to phyllites of the Longobucco Unit was found at Cozzo Vitalba (site n. 8b) [53]. However, it should be specified that these phyllites would belong to the Variscan Bocchigliero Unit, i.e., the late Variscan upper continental crust within the Alpine Sila–Serre Unit [71]. Moreover, the presence of scheelite (W) mineralization in skarns within schists of the contact aureole of the Sila batholith at Croce Reinella (site n. 8c) was documented [107,112,113]. Their genesis was related to the effect of late-Variscan intrusions on pre-existing host rocks [112]. Furthermore, secondary U-minerals autunite and torbernite were found at Vallone Cupone, Cozzo del Principe and Gallopane (site n. 20), within lacustrine sediments overlying magmatic rocks of the Longobucco Unit [54,55].

4.1.2. Corigliano-Rossano (CS) (Sites n. 1–5; Table A1; Figure 2c and Figure 4a)

The presence of Zn-Pb-Fe mineralization considered of hydrothermal origin, occurring north of Longobucco (sites n. 1–5; Table A1; Figure 2c), mostly in veins within the Variscan granitoids close to the contact with phyllites of the Longobucco Unit, is also reported [54,55]. According to the recent literature [100], the phyllites formerly attributed to the Longobucco Unit should belong to the Bocchigliero Unit.
Among the excavation sites for argentiferous galena, the site “Argenteria”, located north of Longobucco towards Corigliano, was reported [17]. In the locality “Baracconi di Campagna—Fonte Argentila” (site n. 5), galena is abundant, possibly associated to minor pyrite in a quartz gangue [110]. Mining tunnels once active at this site for the extraction of Pb are documented [110]. Indeed, positive geochemical anomalies of Pb were detected in this area [47,51]. At Torrente Petraro, strictly close to Fonte Argentila (site n. 5), the mineralizing fluids would have circulated through highly deformed rocks, leading to the formation of mineralized lenses, which are mainly located at the intersection of important fault systems [39,53].
Mineralized veins (sphalerite, galena, pyrite, malachite, and quartz) hosted by granitic rocks of the Longobucco Unit would be located close to the Norman monastery Santuario del Patire (site n. 2) in the Corigliano territory [54]; this site was indicated as one other probable source area for the argentiferous galena [110]. Positive geochemical anomalies of Rb, Cs, Sr, Ta, U, Th, Ce, La, Ba, Nb and Au were detected in the surrounding area of the Patire site [107].
At the mineralized site Cozzo del Pesco (n. 4) in the Corigliano area, pyrite is the most abundant ore mineral, in a quartz gangue, with minor sphalerite veinlets within granodiorites. Porphyry, aplite, pegmatite and microgranite dikes are common at this site [39,53].
In the Rossano area, the mineralization sites reported in the literature are: (i) Torrente Grammisate (site n. 1), where a 30 cm wide mineralized dike (sphalerite, galena, chalcopyrite, fluorite) hosted by granitic rocks of the Longobucco Unit was found at 250 m a.s.l [39,53,55]; (ii) Cerasaro (site n. 3), located to the south-east of Cozzo Chinico, where a 4 m wide dike mineralized by pyrite in quartz gangue was found hosted by granodiorites [39,53,54,55]. The Rossano area would be also characterized by the presence of W-Zn-Cu skarns within the contact aureole of the late-Variscan granitoid, similar to those observed at Longobucco and Savelli [112]. Positive geochemical anomalies of Pb, Zn, Cu, W and Sn were detected in the Rossano area [47].
The mineral association pyrite, chalcopyrite, sphalerite, galena, arsenopyrite, pyrrhotite, electrum, Bi-tetrahedrite, native bismuth, Bi-Ag sulfosalt (pavonite type) and possibly montroydite, in a dominant quartz gangue, characterizes mineralized Fe-Cu-Zn-Pb-As-Bi-Au-Ag-bearing vein samples from an undefined area to the west of Rossano [108]. Two mineralization stages were identified: (i) pyrite + arsenopyrite + base-metal sulphides + quartz; (ii) Bi-tetrahedrite + pavonite + native bismuth + electrum + quartz. The element Au was hosted by arsenopyrite, and mostly by electrum, the latter typically occurring along fractures and in nuggets within pyrite. The first mineralization stage took place under a temperature range of 300–350 °C, and a pressure of 1.5 kbar, based on chemical analyses, whereas an upper thermal limit of 270 °C was inferred for the second stage from the presence of native bismuth [108]. Moreover, fluid inclusion analyses performed on stage II-quartz showed a 135–185 °C range for the minimum temperature of formation and a maximum temperature of 250 °C, with salinities of 6.8–7.3 wt% NaCl eq., for the second stage ore-forming fluid [108]. These results allowed the authors to trace some similarities with gold-bearing veins closely related to late-Variscan granitoids of the French Massif Central [108].

4.2. San Giovanni in Fiore-Savelli-Cerenzia Area

4.2.1. San Giovanni in Fiore (CS) (site n. 12; Table A1; Figure 2c and Figure 4a)

At the San Giovanni in Fiore site, galena and pyrite mineralization within granitic rocks, locally encrusted by meta-autunite, is documented [3,114]. Positive geochemical anomalies of Mn, Y, Cr, Fe, As, Co, Cu, Ni and Sb were detected to the north-east and east of San Giovanni in Fiore, within tonalite, granodiorite and monzogranite intrusions [107].

4.2.2. Serra Toppale-Savelli (KR) (Sites n. 9, 10a, 10b, 10c; Table A1; Figure 2c and Figure 4a)

In the nearby of Savelli, an important mining site was located at Serra Toppale (n. 9), where galena, pyrite and sphalerite mineralized veins cross-cut Variscan granitoids, close to the contact with phyllites [54].
Moreover, in the Savelli area, the following mineralization are documented: (i) pyrite mineralization (site n. 10a), hosted by hornfels near the contact with granodiorites [39,53,55]; (ii) W-Zn-Cu skarns (site n. 10b), within contact aureoles of the late-Variscan granitoid intrusion, similar to those observed at Longobucco and Rossano [112]; (iii) at Torrente Sanapite (site n. 10c), chalcopyrite, malachite, galena and pyrite in pegmatitic dikes, injecting paragneisses near the contact with granodiorites [53].

4.2.3. Cerenzia-Castelsilano (KR) (Sites n. 11, 13; Table A1; Figure 2c and Figure 4a)

The Cerenzia territory has been interested by poor minerary exploitation [53]. Mineralized dikes hosted by granitic rocks of the Longobucco Unit, mainly consisting of galena, sphalerite, pyrite, chalcopyrite and arsenopyrite ore minerals (site n. 13), with quartz, calcite and fluorite gangue minerals, were reported [39,52,53,54]. Anyway, prospection excavations conducted up to the second post-war period, led to the conclusion that this area was not of economic interest [52]. Moreover, a 200 m long molybdenite dike, hosted by granitic rocks of the Longobucco Unit, was reported at Vallone San Lorenzo (site n. 11), in the Cerenzia-Castelsilano area [115], even though subsequent prospection studies were not able to confirm this finding [53].

4.3. Catanzaro-Tiriolo-Gimigliano Area

4.3.1. Molino Mastricarro, Fiumarella (CZ) (Site n. 14; Table A1; Figure 2c and Figure 4a)

A baryte mineralization outcropping along the left bank of the Fiumarella river at Molino Mastricarro (Catanzaro) was reported for the first time in 1878 [15,16], occurring within green and red porphyritic rocks [11,12]. At this site, numerous pegmatites, aplites and lamprophyres frequently crosscut the granitic and metamorphic (phyllites) rocks [36]. A large baryte vein up to 80 m in length and 3 m thick, possibly formed by mineralizing fluids circulating through principal joints within a granitic body, was described [36]. The same fluids also percolated the wall-rocks along fractures, producing several minor veinlets of baryte. All these rocks seem to have suffered intense modifications, not of supergene origin [36]. The minerographic study showed that: (i) the vein mainly consists of spathic baryte, which, in turn, contains nodules and small veinlets of galena, occasionally associated to chalcopyrite and quartz; (ii) the baryte mineralization should have preceded the galena-chalcopyrite-quartz one [36]. Other minor minerals (fluorite, anglesite, pyrite, cerussite, calcite, wulfenite, delafossite, covellite, malachite, azurite, limonite, prehnite, linarite and connellite) were also reported from this deposit [17,36,116,117,118]. Geochemical anomalies of W (>23 ppm) and Zn (>120 ppm) were found for this area [51]. The baryte mine was exploited by the end of the 1960′s and continued until the beginning of the 1980′s of the 20th century, with a production of 25,000 ton/year with a yield of 40% barite [106]; after that, the ore deposit was declared depleted. This mineralization was classified as vein-type pre-Alpine within granitic and porphyritic rocks of the Stilo Unit [54]. The phyllites formerly assigned to the Stilo Unit, should be included in the Bocchigliero Unit [100].
A pioneering fluid inclusion study was performed on the baryte samples from the Molino Mastricarro mine [106], to ascertain whether this deposit could be classified as porphyry Cu-Mo type. The minerographic analysis confirmed the previously observed paragenetic sequence, i.e., the sulphides formed after baryte. The fluid inclusion analyses revealed a minimum range of temperature 190–235 °C, with a salinity of the mineralizing fluids 0–19.5 wt% NaCl eq., and an estimated average minimum pressure of 18.04 bars, for the formation of the baryte mineralization. Based on these results, the genesis of the Fiumarella deposit was put in relation either to epithermal precious metal (with base metals) vein deposits, or to the Kuroko type (i.e., volcanogenic massive sulphides) deposits; either way, excluding the porphyry Cu-Mo hypothesis [106]. This finding would differentiate the Molino Mastricarro mineralization with respect to other deposits occurring within plutonic rocks formerly belonging to the Stilo Unit (e.g., Bivongi in the Serre Massif, namely the Serre Batholith), which are characterized by the presence of molybdenite among their mineral association [54].

4.3.2. Tiriolo (CZ) (Site n.15; Table A1; Figure 2c and Figure 4a)

At the end of the 19th century, one of the most important mineral deposits of the Calabria region was located near the Tiriolo village. Fe-Cu-Zn-ore minerals (pyrite, chalcopyrite, sphalerite, limonite, tetrahedrite and bornite) were collected for the first time in 1878–1887 [15,17,19,20], associated to other minerals (calcite, spinel, garnet, vesuvianite, epidote, chlorite, malachite, azurite, aurichalcite, prehnite, brandisite, fassaite and mesolite) [15,17,19,20,24,25,119,120]. It is worth noting the presence of a green-blue coloured Zn- and Fe3+-bearing spinel, as revealed by chemical, spectroscopic and X-ray diffraction studies [120,121,122,123], in accordance to the observed correlation existing between the blue-green colour and the Fe3+-content of Zn-bearing spinels [124,125]. According to Lovisato [15,17,19], the major ore deposit is hosted by the Paleozoic limestones interleaved to schists, and in close relation to porphyritic magmatic intrusions. However, Panichi [24,25] just reported that the mineral deposit of Tiriolo was found “at the contact between crystalline and overlying carbonate rocks”. According to De Angelis et al. [122], the ore deposit is hosted by thermo-metamorphosed limestones close to granites and tonalites, cross-cut by porphyritic dikes. Following Crisci and Dattola [126], the ore would be hosted by calciphyres produced by thermometamorphism in the presence of fluids at the contact between the magmatic intrusion and pre-existing carbonate rocks.

4.3.3. Gimigliano (CZ) (Site n. 16; Table A1; Figure 2c and Figure 4a)

In the Gimigliano area, a pyrite ore located along the slope of Colle Stretto and at the basis of Colle Pallone, in-between the Amato and Corace rivers, was reported [23,28]. Pyrite was embedded within quartzites intercalated with phyllite schists, and in masses up to 100 m wide and 7 m thick overlying the phyllites, in close relation to the granitic body [28]. A total amount of 100.000 tons of pyrite, with a sulphur content of 47%, was estimated for this ore deposit [28]. Excavation and extraction activities in this area were started in the 1920′s, with the main works being located at the site Cozzica (along the slope of Colle Stretto), and continued up to 1946 [2,28,53]. Concerning the genesis of this pyrite ore, different hypotheses have been put forward: (i) it might be strictly linked to the granite intrusions, as it was already observed in the case of some other sites in Calabria, such as Pazzano, where pyrite is found between limestones and schists close to the granite intrusion [28,29]; (ii) it might be linked to sedimentary and metamorphic processes [53,54,55,109].
In the Gimigliano area, a mineralized site at the Acqua Bollita locality was also reported, which is characterized by the presence of a ferruginous-arsenical water coming from phyllite schists hosting As-bearing pyrite, galena and stibnite mineralization [14,15,18,23].

5. Mineralizations in the Serre Massif in an Updated Geological Framework

In this section, the scientific literature on two major areas of historical mining interest in the Serre Massif is reviewed: (i) Stilo-Pazzano-Bivongi; (ii) San Todaro-Calatria-Caulonia. Data on geochemical anomalies for specific metal elements in some localities [47,51] are detailed. Some information from the literature on the amount of metallic minerals once extracted was also reported for some mining sites. The list of mineralization sites in the Serre Massif is shown in Table A2, where we report a summary of the available literature information and, in the last column, a review of the occurrences of mineral deposits with respect to the current tectono-magmatic and -metamorphic units. The same mineralization sites are indicated on the geological map (Figure 3) and stratigraphic column (Figure 4b).

5.1. Stilo-Pazzano-Bivongi Area (Sites n. 21, 22a, 22b, 22c, 23b, 24a, 24b; Table A2; Figure 3 and Figure 4b)

Positive geochemical anomalies of Pb, As, Zn and Mo were found to the west of the Stilo village [47], where Fe-Ag-Pb-Au-Mn-Cu ore deposits were reported (e.g., [26], and references therein). Particularly noteworthy for economic issues, the limonite mine near to the Stilo and Pazzano villages (site n. 24b) produced 40–45% of Fe on average, which was worked at the metallurgical plant of Ferdinandea [17]. The limonite-goethite-hematite mineralization mainly occurs along the contact between Paleozoic phyllites and Mesozoic limestones (between Monte Stella and Monte Gallo localities), and also fills fractures that cut Jurassic to Cretaceous limestones. This mineralization would be of sedimentary/supergene origin, derived from the oxidation of pre-existing minerals (pyrite, sphalerite, chalcopyrite and galena), and Alpine in age [28,38,54,55].
Differently, according to Vighi [38], the sulphide mineralization hosted by granitic rocks and Paleozoic phyllites, cropping-out along the whole eastern border of the Serre Massif, would be late Carboniferous in age, because it is possibly genetically linked to the Variscan magmas emplacement.
In the area of the Pazzano and Bivongi villages, molybdenite mineralization is primarily hosted by granitoid rocks ([38], and references therein), and in some cases also by the nearby phyllite schists [23,26]. One of the major mining sites in this area was Cantiere Giogli (site n. 22b), which was exploited from 1937 to 1943, and was characterized by a molybdenite vein-type mineralization in a quartz gangue, with minor pyrite, chalcopyrite, limonite, covellite, U-molybdate and ferrimolybdite [26,38,127,128,129]. The mineralized dikes (up to 25 cm thick) were considered of pneumatolytic origin, formed at elevated temperatures, for several reasons: (i) they are interpenetrated with the host quartz-monzonite rock, with gradual transition; (ii) the molybdenite crystals within dikes are often more than 1 cm in size; (iii) small molybdenite crystals are found also within the quartz-monzonite host rocks, often far away from the mineralized dikes [38]. This ore was not considered of economic importance because of its low molybdenite content, i.e., about 5% [38]. According to Bonardi et al. [54], the pneumatolytic-hypothermal molybdenite-pyrrothite mineralization hosted by granitic rocks of the formerly Stilo Unit indicates a deep origin within the continental crust, because the presence of Mo suggests assimilation of large portions of continental crust by the magma and associated fluids.
At the Argostile site (n. 22c), in the nearby of Monte Campanaro locality in the Stilo village area, a pneumatolytic mineralized vein (arsenopyrite, orpiment, quartz), hosted by quartz-monzonite close to the contact with the Palaeozoic schists, crops-out with a lenticular section up to 1 m wide [38]. For the same Argostile locality, a late Variscan galena-sphalerite-arsenopyrite mineralization of hydrothermal origin, hosted by granodiorites, is also reported [55].
At the Serravetta locality, close to the Bivongi village, a pyrite-chalcopyrite ± sphalerite mineralization occurs along the right bank of Torrente Pardalà (site n. 22a), as a diffused impregnation zone within the Palaeozoic schists, close to the contact with quartz-monzonite [38]. Old prospection galleries, nowadays collapsed and closed, were excavated at this site. Waste material from the mine, with 25% average sulphide content, was analysed: dominant pyrite of first generation, containing second generation minerals (chalcopyrite, sphalerite, calcite) infilling fractures, was observed [38]. Similarly, moving from Stilo towards the Guardavalle locality, a chalcopyrite-sphalerite-galena mineralization is located in the stream valley of Fiumara Assi (site n. 21), in the form of a diffuse impregnation zone hosted by the Palaeozoic phyllite schists [38].
In the Bivongi village area (site n. 23b), pre-Alpine mineralization within metamorphic rocks of the formerly Stilo Unit occur as small sporadic lenses of pyrite and pyrrhotite (with quartz gangue) hosted by carbonaceous phyllites, and as disseminations of chalcopyrite, pyrite and pyrrothite within basic rocks intercalated with phyllites [54].
In the nearby of Monte Stella locality, in the Stilo village territory (site n. 24a), a dike filling a fracture within Palaeozoic schists, and located at about 2 km from the contact with the granite intrusion, is mineralized by sphalerite, galena and chalcopyrite in quartz gangue, with up to 70% estimated ore mineral content [38].
Finally, geochemical anomalies of Zn (>120 ppm) and As (>93 ppm) were reported [51] in the Monasterace village territory, in-between the Fiumara Assi and Fiumara Stilaro stream valleys.

5.2. San Todaro-Calatria-Caulonia Area (Sites n. 25, 26a, 26b, 27, 28; Table A2; Figure 3 and Figure 4b)

Of particular note, Mo anomalies (>15 ppm) were found in the Serre Massif to the west of the Monasterace village within granodiorites, indicating the presence of Mo-mineralization [51]. Indeed, a molybdenite vein-type mineralization hosted by quartz-monzonite was reported in an area located about 250 m to the north of San Todaro village (site n. 25) [38,54]. Several mining galleries were excavated at this site, which were already collapsed at the end of the 1940′s: the molybdenite content, found in samples from the waste material of the mine, was less than 5% [38]. Similarly, a few centimetres thick quartz-molybdenite dikes, hosted by heavily fractured and altered quartz-monzonite, were observed at about 250 m to the N-NW of the Calatria village (site n. 26a), inside mining galleries [38].
Moreover, Vighi [38] studied a mineralized site located at 1.1 km to the N-E of the Calatria village (site n. 26b), with a vertical dike within phyllites, close to the contact with granites. The paragenetic sequence: pyrrhotite, marcasite, pyrite + quartz, sphalerite + calcite + chalcopyrite + galena, calcite II + pyrite II + quartz II, was suggested for this mineralization. A maximum temperature of about 450 °C was estimated for the marcasite formation [38]. Pre-Alpine stratabound chalcopyrite mineralization, as disseminated lenses hosted by carbonaceous phyllites of the formerly Stilo Unit, is reported at the Monte Granieri locality, in the Calatria village territory (site n. 27) [54].
Finally, an As-Cu-Fe vein-type mineralization (arsenopyrite, pyrite, and chalcopyrite, in a quartz gangue) was found at the San Blasio locality, in the Caulonia territory (site n. 28), hosted by metamorphic rocks close to the contact with the Variscan granodiorites of the formerly Stilo Unit [54].
In the need to review the tectonic units hosting the above-described mineralization in the Serre Massif, in an updated geological framework, we can observe that such mineralization is distributed within the intermediate and upper portions of the late Variscan continental crust block (Figure 4b), i.e., within the Sila-Serre Unit [71]. The mineralization at sites n. 22b, 23a, 25 and 26a (Table A2; Figure 3 and Figure 4b), occurring in granitoids previously assigned to the Stilo Unit (e.g., [54,126]), can be located in the intermediate crust; they might be considered genetically linked to the late Carboniferous intrusive magmatic events, which gave rise to the Serre batholith (e.g., [78,91]). The mineralization at sites n. 21, 22a,c, 23b,c, 24a,b and 26b-28 (Table A2; Figure 3 and Figure 4b), occurring in igneous and metamorphic rocks, formerly assigned to the Stilo Unit (e.g., [54]), are located in the upper crust. They might be related to hydrothermal activity and/or contact metamorphism at the roof of the Serre batholith (e.g., [92]), or to the late Carboniferous-Permian dike magmatism [93,101].

6. Discussion, Open Issues and Future Directions

Our overview of the known literature on the mineralization of the Sila and Serre Massifs allowed us to evidence some critical aspects, and also to highlight some open issues which are worth dealing with, in order to deepen the understanding on this topic.
First of all, the literature on this subject is definitely not exhaustive and mostly out-of-date, mainly consisting of a few old scientific papers (e.g., [56], and references therein), and some archeo-minerary papers from which it is not clear whether the reports of mineral findings are based on direct analytical evidence made by the authors or not (e.g., [110]). Difficulties may sometimes arise when trying to exactly locate the mineralized sites on the geological and topographical maps, just based on reports found in the old literature. This happens for many reasons, among which is the proliferation of several slight differences in the way by which the same toponym name has been transmitted through time in the different papers; moreover, the presence of geographically distinct sites having similar toponyms (e.g., Reinella, Reginella, Righinella, and Reghinella, in the Longobucco area) gives rise to further confusion. In some cases, field prospections intended to verify the early reports on mineralization occurrences did not confirm those notices [130,131]. In this respect, it is of particular interest that many indications of the presence of gold in several localities in the Calabria mineralizing province were not subsequently confirmed. This led to the suggestion that, in past times other minerals, such as pyrite and altered biotite, might have been misleadingly identified as gold [130]. In the same stream, the recurrent difficulty of finding the famous argentiferous galena, encountered by several authors in different mining sites of Calabria (e.g., [5,23,37]), is also worth exploring further and clarifying.
The main open question emerging from our overview is the need for a deeper analysis of the genesis of these ore deposits. According to the old literature, every mineralization of the Sila and Serre Massifs occurred within continental derived units, and most of them were genetically linked to the late-Variscan magmatic intrusions; mineralization occurrences related to sedimentary and metamorphic processes were sporadically found [53]. Two distinct mineralization episodes were suggested for the Serre Massif: (i) slightly later than the Variscan intrusion; (ii) linked to the Alpine orogenesis [38]. According to Vighi [38], a marked lateral zoning would characterize mineralization occurrences in the Serre Massif, with high temperature molybdenite-quartz dikes hosted by quartz-monzonite of the inner parts, and low temperature sphalerite-galena-chalcopyrite-quartz dikes occurring within phyllites of the outer parts; such lateral zoning would testify that the formation of these mineral deposits closely followed the granitic intrusion [38]. To this concern, our review of the host tectonic units has allowed us to locate mineralization of the Serre Massif within a stratigraphic column (Figure 4b), from which it is apparent that the molybdenite ore deposits (e.g., sites n. 22b, 23a, 25, 26a; Table A2; Figure 4b) are deeper and located in the intermediate portion of the Variscan continental crust, whereas the other ones are located in the upper crust (Figure 4b).
According to Bonardi et al. [54], apart from a few recent mineralizations, mainly pre-Alpine mineralized systems occurred in Calabria, which would have been split-up during the Alpine evolution, and found in a fragmentary way in the present orogenic structure. Even though some genetic hypotheses have been put forward by a few authors in the early literature (e.g., [53,54]), such hypotheses cannot be considered exhaustive at all. Some similarities about the geological context in which the Sila and Serre mineral deposits formed can be derived just from the overview of the previous literature, such as the frequently observed close relation of the mineralization with the Variscan intrusive granitic bodies and with their associated late stage and shallower porphyritic dikes (e.g., [15,16,37,53,54]). In addition, an interesting correlation between mineralizations and the highly faulted structural setting of the host rocks appears when trying to locate the mineralization reports on the geological maps. Moreover, several polymetallic mineralizations of the Sila and Serre Massifs show some common features with specific European ore deposits, ascribed to a post-Variscan and late Carboniferous-Permian geodynamic context. These similarities are attributed to the variety of intrusive magmas which are associated to the mineralization (i.e., granites and monzogranites, expression of late S-type and K-type Variscan magmatism; leucogranites, lamprophyres and andesitic dikes, ascribed to late-Carboniferous to Permian A-type magmatism) (e.g., [132,133]). The chemical differences recorded in the Calabrian mineralization might possibly be the consequence of several overlapping genetic processes, even though some groups of ore deposits also present in other European contexts may be identified. In detail, the main Zn-Pb-Fe-Cu vein-type mineralization, found in the Longobucco, Rossano, Savelli and Stilo-Bivongi areas, is also observed in the French Central Massif [134,135], in the Freiberg District and Harz Mountains in Germany [136,137,138,139], in the Kutna Hora District in the Czech Republic [140], and in the Sulcis and Arburese areas of Sardinia [141,142,143]. All these ore deposits are related to post-Variscan and late Carboniferous to Permian magmatic-hydrothermal events. Post-Variscan mineralization events are also documented in Europe, e.g., the Middle Permian and Mesozoic ones in southern Sardinia [144].
Indeed, a more detailed study could help to constrain the genetic conditions and to highlight any possible correlation among different mineralization sites/events, also with the aim of ascertaining such a largely accepted supposed connection of the Calabrian mineralization with those found in other European regions with similar geological context, such as Sardinia and the French Central Massif (e.g., [56,108,112]. In addition, detailed research of the Calabrian ore deposits might contribute to better understanding the possible association of the Calabria geodynamic context with that of other European Variscan Massifs.
In this respect, the spatial relationship existing between most of the Calabria ore mineralizations and the late Variscan intrusions was observed by several authors (e.g., [53,55]), even though their genetic connection is still to be analytically proved. The hypothesis put forward in past times of a genetic link to porphyry type deposits was discarded based on fluid inclusion studies, at least for the Sila mineralization occurrences [106,107,108]. In particular, a wide range of temperatures (50–416 °C) and salinities (0–26 wt.% NaCl eq.) were observed for fluid inclusions entrapped within magmatic rocks from different sites of the Sila batholith [107]. It was suggested that the highest temperatures might correspond to magmatic-related Variscan fluids, and the lowest ones to fluids of either Variscan or Alpine age. Fluids typical of porphyry systems were not observed [107]. In spite of this, the possibility that non-porphyry fluids were linked to the Variscan intrusions, because they at least suffered their heating effects, is another genetic hypothesis to be verified. Moreover, a further possibility is that the ore deposits are chronologically subsequent to the Variscan intrusions. All these hypotheses require verification by means of scientific-analytical studies, considering that one other big open question just deals with the lack in dating studies of the ore mineralization. Furthermore, the conclusions proposed by some authors (e.g., [55]) that primary concentrations of ore minerals genetically linked to Variscan intrusions were subsequently dispersed by the Alpine metamorphism, and that the scarcity of ore mineralization in the Alpine ophiolitic units (e.g., in the Gimigliano Unit) might be partly due to this effect, are still to be verified.
Strictly linked to the genetic topic, scientific studies aimed at unravelling the relationships existing between the vein-type mineral deposits and the tectonic evolution, leading to the formation of the mineralized fractures, are still needed and represent future perspectives.
The mining industry in the Sila and Serre areas has always been poor and concentrated in a few sites, especially in the Stilaro valley and in the Longobucco area, mainly because of the inaccessible nature and transport difficulties of those regions that made the extractive activities too much expensive, and also considering the small ore volumes [8,28,37]. Furthermore, even though the old literature came to the conclusion that the Calabria-Peloritani Arc was to be considered a barren region due to the small size of its mineralizations [56], a renewed economic interest in these areas may arise by considering the possibility that sphalerite occurrence in historical mining districts may represent an attractive target for critical metals such as Ge, Ga and In [143]. Indeed, a wide range of minor/trace elements (including Ga, Ge, In) can substitute for Zn in sphalerite, and, in some cases, these elements are extracted as by-products during sphalerite processing [145]. For example, the sphalerite of the main Ge deposit in western Europe, the vein-type Zn–Ge–Ag–(Pb–Cd) deposit of Noailhac-Saint-Salvy (Tarn, France), contains up to 2600 ppm Ge [135,146].
In our opinion, in spite of the “scarce” economic potential of the Calabria ore deposits, their importance from a scientific view point must still be preserved and appreciated. Scientific analytical data have been published only for a few mineralization sites. In many cases, the available data were collected a long time ago and presented in pioneering papers (e.g., [106]). In the majority of cases, studies were abruptly ceased at the beginning of the 1990′s (e.g., [108]), possibly because of the declared loss of economic interest for extractive activities in these areas. In a few recent cases, renewed scientific interest for the Calabria mineralization led to the publication of short analysis reports (e.g., [117,118]), with a great temporal gap with respect to the older literature. This led to a considerable open space for further analytical research on these mineral deposits, with the aim of a proper characterization, possibly leading to ascertaining genetic hypotheses on their formation.

Author Contributions

Conceptualization, V.F. and R.A.F.; investigation, R.A.F., A.C. and F.T.; resources, R.A.F., A.C. and F.T.; writing—original draft preparation, R.A.F. and A.C.; writing—review and editing, R.A.F., A.C., V.F., G.R., F.T., E.S. and G.V.; visualization, A.C., V.F., F.T. and R.A.F.; project administration, R.A.F.; funding acquisition, R.A.F. and A.C. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by Università degli Studi di Bari Aldo Moro, grant numbers U.P.B. FregolaRicerca15-16, and U.P.B. FregolaRicat17-18 to R.A.F.; Ph.D. grant to A.C.

Data Availability Statement

Data are contained within the article.

Acknowledgments

We are grateful to three anonymous reviewers, whose comments and suggestions helped us to improve the original draft of the manuscript. The Editors are thanked for the handling of the manuscript.

Conflicts of Interest

The authors declare no conflict of interest. The funders had no role in the design of the study; in the collection, analyses, or interpretation of data; in the writing of the manuscript; or in the decision to publish the results.

Appendix A

Table
Table A1. Mineralization sites and geological framework of the Sila Massif.
Table A1. Mineralization sites and geological framework of the Sila Massif.
Literature DataReview
Mineralization Type (**)No.LocalityOre
Deposit		Ore
Minerals		Gangue MineralsHost Rock and Old
Tectonic Unit		Assumed GenesisReferencesContemporary
Tectonic Unit
Pre-Alpine
within
magmatic rocks		1Torrente Grammisate
(Rossano)		Zn-Pb-Fe-Cusp, gn, ccp,flrveins within Variscan granitoids close to the contact with phyllites;
Longobucco Unit		hydrothermal[39,53,55]Sila-Serre Unit,
Batholith
2Santuario del Patire (Corigliano)Zn-Pb-Fe (*)sp, gn, pyqz[54,110]Sila-Serre Unit,
Batholith
3Cerasaro-Cozzo Chinico (Rossano)Fepyqz[39,53,54,55]Sila-Serre Unit,
Batholith
4Cozzo del Pesco (Corigliano)Fe-Zn-Pbpy, sp, gnqz[39,53,54,55]Sila-Serre Unit, Batholith and Bocchigliero/
Stilo-Pazzano Unit
5Baracconi—Fonte Argentila—Torrente Petraro
(Corigliano)		Pb (*)gn, (py)qz[39,53,54,55,110]Sila-Serre Unit,
Batholith
6Difesella del Trionto
(Longobucco)		Zn-Pbsp, gncal[54,55]Sila-Serre Unit,
Batholith
7Croce della Reghinella—Macchiafarna—Fiume Trionto (Longobucco)Zn-Pbsp, gnn.d.[54]Sila-Serre Unit, Batholith and Bocchigliero/
Stilo-Pazzano Unit
8aTorrente La Manna—
Torrente Macrocioli—
M. Cerzito—Cozzo Vitalba—Fosso Belvedere
(Longobucco)		Zn-Fe-Pb-Cu (*)sp, gn, py, ccpflr[53,54]Sila-Serre Unit, Batholith and Bocchigliero/
Stilo-Pazzano Unit
9Serra Toppale (Savelli)Pb-Zn-Fe (*)gn, sp, pyn.d.[54]Bocchigliero/
Stilo-Pazzano Unit
Pre-Alpine within magmatic rocks11Vallone San Lorenzo
(Cerenzia-Castelsilano)		Momoln.d.veins within
granitoids close to
phyllites;
Longobucco Unit		hydrothermal[53,54,55,115]Sila-Serre Unit,
Batholith
13Cerenzia—CaccuriPb-Zn-As-Fe-Cugn, sp, py, apy, ccpqz, flr, cal[29,52,53,54]Sila-Serre Unit,
Batholith
12San Giovanni in Fiore (CS)Pb-Fe (U)gn, py,
(maut)		flrgranitic rocks
(incrustation)		n.d.[3,29,114]Sila-Serre Unit,
Batholith
14Molino Mastricarro
(Catanzaro)		Ba (*)-Pb-Cubrt, gn, ccpqz, flrveins within granitic and porphyritic rocks; Stilo Unitepithermal[15,16,17,36,54,55,106,116,117,118]Sila-Serre Unit,
Batholith
Pre-Alpine within metamorphic rocks8bCozzo Vitalba
(Longobucco)		Fepyn.d.veins in carbonatic lenses intercaleted to phyllites;
Longobucco Unit		n.d.[53]Bocchigliero/
Stilo-Pazzano Unit
8cCroce Reinella
(Longobucco)		Wschn.d.skarns in phyllites;
Bocchigliero Unit		n.d.[107,112,113]Bocchigliero/
Stilo-Pazzano Unit
10aSavelliFepyn.d.hornfels;
Bocchigliero Unit		contact-
metamorphic.		[39,53,55]Mandatoriccio/
Mammola Unit
10bSavelliW-Zn-Cun.d.n.d.skarnscontact-
metamorphic		[112]Mandatoriccio/
Mammola Unit
10cTorrente Sanapite
(Savelli)		Cu-Fe-Pbccp, mlc, gn, pyn.d.pegmatitic dikes in paragneiss;
Mandatoriccio Unit		n.d[53]Mandatoriccio/
Mammola Unit
15TirioloFe-Cu-Znpy, ccp, sp, ttr, bn, mlc, lmn.d.meta-carbonate rocks close to the granite
intrusion;
Stilo Unit		n.d.[15,17,19,20,24,25,29,53,122,126]Sila-Serre Unit,
Lower Crust
16Colle Stretto, Colle Pallone, Fosso Patia
(Gimigliano)		Fe (*)pyn.d.phyllites and phyllitic quartzites;
Bagni Unit		sedimentary; metamorphic[2,28,29,53,54,55,109]Fiume Pomo Unit
Pre-Alpine
within
metamorphic rocks		17S. Pietro Apostolo,
Martirano, Conflenti		Fepyn.d.metamorphic rocks;
Bagni Unit		metamorphic[28,54,126]Fiume Pomo Unit
18Platania (CZ)Fepyqzlenses in quartz-rich phyllites;
Bagni Unit		hydrothermal[29,53,55,130,131]Fiume Pomo Unit
19Serra Pedace (CS)Pb, (Ag)(Ag)-gnn.d.phyllitesn.d.[23]Sila-Serre Unit,
Lower Crust
Recent20V.ne Cupone-Cozzo del Principe-Gallopane (Longobucco)Uaut, torn.d.lacustrine sediments; Longobucco Unitsedimentary (secondary)[54,55]Sila-Serre Unit
(Quaternary sediments)
Notes: The table includes all the available literature information. The lack of detailed information regards, e.g., the host rock (sometimes metamorphic rocks are generically reported), and the assumed genesis of the mineral deposit. (*) Historically mined; (**) in relation to the Alpine orogenesis and host rock; n.d. = not defined. Mineral symbols: apy (arsenopyrite), aut (autunite), maut (meta-autunite), bn (bornite), brt (baryte), cal (calcite), ccp (chalcopyrite), flr (fluorite), gn (galena), lm (limonite), mlc (malachite), mol (molybdenite), py (pyrite), qz (quartz), sp (sphalerite), sch (scheelite), tor (torbernite), ttr (tetrahedrite).

Appendix B

Table
Table A2. Mineralization sites and geological framework of the Serre Massif.
Table A2. Mineralization sites and geological framework of the Serre Massif.
Literature DataReview
Mineralization Type (**)No.LocalityOre
Deposit		Ore
Minerals		Gangue MineralsHost Rock and Old
Tectonic Unit		Assumed
Genesis		ReferencesContemporary
Tectonic Unit
Pre-Alpine within
magmatic rocks		22bCantiere Giogli (Pazzano, Bivongi)Mo (Cu, Fe, U) (*)mol, py, ccp, cv, lm, fmyb,
U-molybdate		qzmineralized dikes in quartz-monzonitepneumatolytic[26,38,127,128,129]Sila-Serre Unit,
Batholith
22cArgostile (Stilo)Fe-As (Pb-Zn)apy, orp
(gn, sp)		qzmineralized dike in quartz-monzonites (granodiorites), close to the contact with schistspneumatolytic; (hydrothermal)[38,55]Sila-Serre Unit, Batholith and Bocchigliero/
Stilo-Pazzano Unit
23aBagni di Guida, Stilaro (Bivongi)Mo
(Cu-Fe)		mol,
(ccp)		n.d.magmatic rocks;
Stilo Unit		hydrothermal[54]Sila-Serre Unit,
Batholith
25San TodaroMo (Cu-Fe) (*)mol, (ccp)n.d.quartz-monzonite;
Stilo Unit		hydrothermal[38,54]Sila-Serre Unit,
Batholith
26aCalatriaMo (*)molqzdikes in
quartz-monzonite;
Stilo Unit		hydrothermal[38]Sila-Serre Unit,
Batholith
Pre-Alpine within metamorphic rocks
21Fiumara Assi (Guardavalle, Stilo)Fe-Cu-Zn-Pbccp, sp, gnn.d.impregnation zone
in Paleozoic schists		n.d.[38]Bocchigliero/
Stilo-Pazzano Unit
22aSerravetta,
Torrente Pardalà (Bivongi)		Fe-Cu-Zn (*)py, ccp, spcalimpregnation zone in Paleozoic schists, close to the contact with quartz-monzoniten.d.[38]Sila-Serre Unit, Batholith;
Bocchigliero/
Stilo-Pazzano Unit
23bBivongiFe-Cupy, po, ccpqzlenses in carbonaceous phyllites/disseminations in basic rocks
intercalated with
phyllites; Stilo Unit		metamorphosed sedimentary/
metamorphosed volcanogenic		[54]Bocchigliero/
Stilo-Pazzano Unit
23cBivongiCu-Feccpqzmetamorphic rocks, close to the contact with granodiorites; Stilo Unithydrothermal[54]Sila-Serre Unit, Batholith;
Bocchigliero/
Stilo-Pazzano Unit
24aMonte Stella (Stilo)Zn-Pb-Cu-Fesp, gn, ccpqzmineralized dike
in Paleozoic schists		n.d.[38]Bocchigliero/
Stilo-Pazzano Unit
26bCalatriaFe-Zn-Cu-Pbpo, mrc, py, sp, ccp, gnqz, caldike in phillites close to the contact with graniten.d.[38]Sila-Serre Unit, Batholith;
Bocchigliero/
Stilo-Pazzano Unit
27Monte Granieri
(Calatria)		Cu-Feccpqzdisseminated lenses in carbonaceous phyllites; Stilo Unitmetamorphosed sedimentary[54]Bocchigliero/
Stilo-Pazzano Unit
28San Blasio
(Caulonia)		As-Cu-Feapy, py, ccpqzmetamorphic rocks, close to the contact with granodiorites; Stilo Unithydrothermal[54]Mandatoriccio/
Mammola Unit
Alpine24bMonte Stella,
Monte Gallo
(Stilo, Pazzano)		Fe
(Cu-Pb-Zn) (*)		lm, gth, hem n.d.at the contact between Mesozoic limestones and Paleozoic phyllites; in fractures across
Jurassic to Cretaceous limestones; Stilo Unit		sedimentary/
supergene		[28,38,54]Longobucco/
Stilo cover
Notes: The table includes all the available literature information. The lack of detailed information regards, e.g., the host rock (sometimes metamorphic rocks are generically reported), and the assumed genesis of the mineral deposit. (*) Historically mined; (**) in relation to the Alpine orogenesis and host rock; n.d. = not defined. Mineral symbols: apy (arsenopyrite), cal (calcite), ccp (chalcopyrite), cv (covellite), fmyb (ferrimolybdite), gn (galena), gth (goethite), hem (hematite), lm (limonite), mol (molybdenite), mrc (marcasite), orp (orpiment), py (pyrite), po (pyrrhotite), qz (quartz), sp (sphalerite).

References

  1. Holwell, D.A.; Fiorentini, M.L.; Knott, T.R.; McDonald, I.; Blanks, D.E.; McCuaig, T.C.; Gorczyk, W. Mobilisation of deep crustal sulphide melts as a first order control on upper lithospheric metallogeny. Nat. Commun. 2022, 13, 573. [Google Scholar] [CrossRef]
  2. Cuteri, F.A. Risorse minerarie ed attività metallurgica nella Sila Piccola e nella Pre-Sila del versante tirrenico. Prime osservazioni. In Tra l’Amato e il Savuto. II. Studi sul Lametino Antico e Tardo-Antico; De Sensi Sestito, G., Ed.; Rubbettino: Soveria Mannelli, Italy, 1999; pp. 293–317. (In Italian) [Google Scholar]
  3. Saccà, C.; Saccà, D.; Nucera, P.; De Fazio, A. Mineralizzazioni in Calabria—Storia e Attualità; Onorati, G., Ed.; Aracne Editrice: Roma, Italy, 2017; p. 131. (In Italian) [Google Scholar]
  4. Franco, D. Il Ferro in Calabria. Kaleidon, Ed.; Reggio: Calabria, Italy, 2003; Volume 176. (In Italian) [Google Scholar]
  5. Franco, D. Le Reali Fabbriche del Ferro in Calabria. Tra Storia e Archeologia Industriale; Rubbettino Editore: Soveria Mannelli (Catanzaro), Italy, 2019; p. 238. (In Italian) [Google Scholar]
  6. Franco, D.; Riggio, S. Memorie Industriali in Calabria. Siderurgia e Metallurgia nelle Serre Calabre; A.C.A.I.: Catanzaro, Italy, 1992; p. 47. (In Italian) [Google Scholar]
  7. Paillette, A. Ếtude historiques et géologiques sur les gítes métallifères des Calabres et du nord de la Sicile. Ann. Mines 1842, II, 613–678. (In French) [Google Scholar]
  8. De Beaumont, E.; Pelouze, T.J.; Dufrénoy, O.P.M. Rapport sur un Mémoire de M. Adrien Paillette, ayant pour titre: Études historiques et géologiques sur le gîtes métallifères des Calabres et du nord de la Sicilie. C. R. Hebd. Acad. Sci. 1842, 14, 323–328. (In French) [Google Scholar]
  9. Cantarelli, F. De’ saggi delle manifatture napolitane nell’anno 1844. Ann. Civ. Regno Due Sicilie 1844, LXVII, 117–169. (In Italian) [Google Scholar]
  10. Pandolfi, O. Sullo stato attuale della illustrazione geologica e mineralogica della Calabria Citeriore. Atti Acc. Cosent. 1861, 8, 81–237. (In Italian) [Google Scholar]
  11. Vom Rath, G. Osservazioni geologiche fatte in Calabria. Boll. R. Com. Geol. Ital. 1873, 11–12, 323–344. (In Italian) [Google Scholar]
  12. Vom Rath, G. Geognostisch-mineralogische fragmente aus Italien. Z. Dtsch. Geolog. Ges. 1873, Bd. 25, 117–248. (In German) [Google Scholar]
  13. Jervis, G. I Tesori Sotterranei Dell’Italia. L’Apennino e i Vulcani Attivi e Spenti Dipendentevi; Loescher: Torino, Italy, 1874; Volume 2, p. 623. (In Italian) [Google Scholar]
  14. Lovisato, D. Cenni geognostici e geologici sulla Calabria settentrionale. Parte I. Boll. R. Com. Geol. Ital. 1878, 9, 155–174, 468–487. (In Italian) [Google Scholar]
  15. Lovisato, D. Il Monte di Tiriolo. Memoria del Dottor Domenico Lovisato (Dalla Cronaca Liceale 1877–78). Tipografia V. Asturi: Catanzaro, Italy, 1878; p. 26. (In Italian) [Google Scholar]
  16. Lovisato, D. Cenni geognostici e geologici sulla Calabria settentrionale. Parte II. Rocce primitive della Sila. Boll. R. Com. Geol. Ital. 1878, 9, 347–363. (In Italian) [Google Scholar]
  17. Lovisato, D. Sulle Chinzigiti della Calabria. Mem. R. Accad. Lincei 1879, III, 221–239. (In Italian) [Google Scholar]
  18. Lovisato, D. Cenni geognostici e geologici sulla Calabria settentrionale. Parte II. Boll. R. Com. Geol. Ital. 1879, 10, 24–39,108–137. (In Italian) [Google Scholar]
  19. Lovisato, D. Il Monte di Tiriolo. Boll. R. Com. Geol. Ital. 1879, 10, 60–62. (In Italian) [Google Scholar]
  20. Neviani, A.I. Minerali del monte tiriolo. In Di Alcuni Minerali Raccolti Nella Provincia di Catanzaro; Tipografia del “Calabro”: Catanzaro, Italy, 1887; pp. 3–9. (In Italian) [Google Scholar]
  21. Neviani, A. II Minerali delle miniere solfifere di Santa Dominica. In Di Alcuni Minerali Raccolti Nella Provincia di Catanzaro; Tipografia del “Calabro”: Catanzaro, Italy, 1887; pp. 10–12. (In Italian) [Google Scholar]
  22. Novarese, V. Calcari cristallini e calcefiri dell’Arcaico calabrese. Boll. R. Com. Geol. Ital. 1893, 24, 17–43. (In Italian) [Google Scholar]
  23. Cortese, E. Descrizione Geologica Della Calabria, 2nd ed.; Casa del libro editrice: Roma, Italy, 1983; p. 338. (In Italian) [Google Scholar]
  24. Panichi, U. Sui minerali del giacimento di Tiriolo (provincia di Catanzaro). I. Il giacimento. Atti R. Accad. Lincei S. V 1911, 20, 421–424. (In Italian) [Google Scholar]
  25. Panichi, U. Sui minerali del giacimento di Tiriolo (provincia di Catanzaro). II. Minerali non prima osservati. Atti R. Accad. Lincei S. V 1911, 20, 518–523. (In Italian) [Google Scholar]
  26. Panichi, U. Molibdenite ed altri minerali di Bivongi e di Pazzano (prov. di Reggio Calabria). Atti R. Accad. Lincei S. V 1911, 20, 654–658. (In Italian) [Google Scholar]
  27. Stella, A. Le miniere di ferro dell’Italia. In Proceedings of the Primo Congresso Minerario Nazionale, Roma, Italy, 10–12 June 1917; Federazione Mineraria Italiana. Lattes: Torino, Italy, 1921; p. 426. (In Italian). [Google Scholar]
  28. Moschetti, A. Giacimenti di pirite di Gimigliano. Min. Ital. 1927, 11, 273–275. (In Italian) [Google Scholar]
  29. Penta, F. Sguardo minerario sull’Italia Meridionale. Ind. Miner. d’Ital. E d’Oltremare 1938, 6, 211–218. (in Italian). [Google Scholar]
  30. Penta, F. Studi geominerari e geotecnici. L’attività svolta dal Centro Studi delle Risorse Naturali dell’Italia Meridionale dal 31 agosto 1940 al 28 ottobre 1941 (III relazione). Atti R. Ist. Inc. Napoli 1941, 84, 75. (In Italian) [Google Scholar]
  31. Ippolito, F. Il Centro Ricerche Geominerarie dell’IRI (Napoli). Experientia 1947, 3, 124. (In Italian) [Google Scholar] [CrossRef]
  32. Rittmann, A. Il Centro di Studi Silani. Sezione Geomineraria; attività svolta durante l’anno 1947. Ric. Sci. E Ricostr. 1947, 17, 12. (In Italian) [Google Scholar]
  33. Rittmann, A. Sull’esistenza di colate riolitiche post-Alpine in Sila. Rend. Lincei VIII 1946, 1, 1206–1207. (In Italian) [Google Scholar]
  34. Ippolito, F. Studi geologici in Calabria. Ric. Sci. E Ricostr. 1947, 17, 54–56. (In Italian) [Google Scholar]
  35. Ippolito, F. Primi risultati di studi geologici eseguiti in Calabria nel 1946. Boll. Soc. Natural. Napoli 1947, LV, 105–107. (In Italian) [Google Scholar]
  36. Vighi, L. Studio di un’area mineralizzata a baritina e solfuri vari in Calabria. Ric. Sci. 1948, 10, 1339–1344. (In Italian) [Google Scholar]
  37. Vighi, L. Sulla geologia e sulle mineralizzazioni metallifere della regione di Longobucco in Calabria. Mem. E Note Ist. Geol. Appl. Napoli 1953, 5, 3–61. (In Italian) [Google Scholar]
  38. Vighi, L. Mineralizzazioni a solfuri misti e ad ossidi di ferro nel bordo orientale della Serra San Bruno, in Calabria. Mem. E Note Ist. Geol. Appl. Napoli 1949, 2, 37–74. (In Italian) [Google Scholar]
  39. CNEN. Relazione Sulla Campagna 1960, Internal Report; Gruppo Delta: Bologna, Italy, 1960. (In Italian) [Google Scholar]
  40. CNEN. Relazione Sulla Campagna 1961, Internal Report; Gruppo Delta: Bologna, Italy, 1961. (In Italian) [Google Scholar]
  41. CNEN. Rapporto di Attività del Gruppo Delta Nell’Anno 1961–62. Internal Report; Gruppo Delta: Bologna, Italy, 1962. (In Italian) [Google Scholar]
  42. CNEN. Relazione Sulla Campagna 1962–63. Gruppo di prospezione. Internal Report; Gruppo Delta: Bologna, Italy, 1963. (In Italian) [Google Scholar]
  43. CNEN. Relazione Sull’Attività Svolta Nel 1967 dal Laboratorio Geominerario, Internal report; CSN, Casaccia: Bregaglia, Switzerland, 1968. (In Italian) [Google Scholar]
  44. Mittempergher, M. Le risorse di torio in Italia. Not. CNEN 1968, 3. (In Italian) [Google Scholar]
  45. RIMIN. Convenzione tra il Ministero dell’Industria, del Commercio e dell’Artigianato e l’Ente Nazionale Idrocarburi-E.N.I., per l’esecuzione di un Programma di Ricerche Minerarie in Calabria. Rapp. Final. 1981; unpublished report. (In Italian) [Google Scholar]
  46. De Vivo, B.; Cavaliere, S.; Lima, A.; Crisci, G.M. Active stream sediments multielemental geochemical survey in the Longobucco area (Calabria). Boll. Soc. Geol. Ital. 1981, 100, 499–525. [Google Scholar]
  47. De Vivo, B.; Closs, L.G.; Lima, A.; Marmolino, R.; Perrone, V. Regional geochemical prospecting in Calabria, Southern Italy. J. Geochem. Explor. 1984, 21, 291–310. [Google Scholar] [CrossRef]
  48. MICA-ENI; Convenzione Programmatica Italia Meridionale. Ministero dell’Industria: Roma, Italy, 1987. (In Italian)
  49. MICA-ENI; Convenzione per la “Valutazione del potenziale metallogenico dei terreni cristallini della Calabria”. Ministero dell’Industria: Roma, Italy,, 1989. (In Italian)
  50. MICA-ENI; Convenzione “Mineralizzazioni legate alle plutoniti dell’Unità di Longobucco e dell’Unità di Stilo”. Ministero dell’Industria: Roma, Italy, 1991. (In Italian)
  51. De Vivo, B.; Costabile, S.; Lima, A. Cartografia geochimica della Calabria. Mem. Descr. Carta Geol. Ital. 1998, LV, 17–29, (In Italian, English abstract). [Google Scholar]
  52. Minniti, M.; Stampanoni, G.; Vighi, L. VII—Calabria. In Memoria Illustrativa Della Carta Mineraria d’Italia. Memorie per Servire Alla Descrizione Della Carta Geologica d’Italia; Castaldo, G., Stampanoni, G., Eds.; MICA—Ministero dell’Industria del commercio e dell’artigianato, Servizio Geologico d’Italia, Stabilimento tipografico Ugo Pinto: Roma, Italy, 1975; Volume XIV, pp. 145–160. (In Italian) [Google Scholar]
  53. De Vivo, B.; Lorenzoni, S.; Orsi, G.; Zanettin Lorenzoni, E. Inquadramento delle mineralizzazioni metallifere ed a grafite nelle unità tettoniche della Calabria. Primo contributo: La Sila e le Serre. Ind. Miner. 1978, 29, 108–120. (In Italian) [Google Scholar]
  54. Bonardi, G.; De Vivo, B.; Giunta, G.; Lima, A.; Perrone, V.; Zuppetta, A. Mineralizzazioni dell’Arco Calabro-Peloritano. Ipotesi genetiche e quadro evolutivo. Boll. Soc. Geol. Ital. 1982, 101, 141–155, (In Italian, with English abstract). [Google Scholar]
  55. Lorenzoni, S.; Orsi, G.; Zanettin Lorenzoni, E. Metallogenesis in the tectonic units and lithogenetic environments of Calabria (Southern Italy). Mem. Sci. Geol. 1983, 35, 411–428. [Google Scholar]
  56. Zanettin Lorenzoni, E.; Zuffardi, P. Geo-tectonic evolution and metallogenesis of the Calabrian-Peloritanian Arc in the Tethys realm. In Proceedings of the Final Symposium of IGCP Project 169, Leoben, Austria, October 1984; Petrascheck, W.E., Jankovic, S., Eds.; Springer: Wien, Austria, 1986; pp. 175–192. [Google Scholar]
  57. De Vivo, B.; Lorenzoni, S.; Zanettin-Lorenzoni, E.; Orsi, G. Le mineralizzazioni nel basamento cristallino dell’Aspromonte (Calabria). Boll. Soc. Geol. Ital. 1980, 99, 289–302. (In Italian) [Google Scholar]
  58. Bonardi, G.; Cavazza, W.; Perrone, V.; Rossi, S. Calabria-Peloritani Terrane and Northern Ionian Sea. In Anatomy of an Orogen: The Apennines and Adjacent Mediterranean Basins; Vai, G.B., Martini, I.P., Eds.; Kluwer: Dordrecht, The Netherlands, 2001; pp. 287–306. [Google Scholar]
  59. Amodio-Morelli, L.; Bonardi, G.; Colonna, V.; Dietrich, D.; Giunta, G.; Ippolito, F.; Liguori, V.; Lorenzoni, S.; Paglionico, A.; Perrone, V.; et al. L’Arco Calabro-Peloritano nell’orogene Appenninico-Maghrebide. Mem. Soc. Geol. Ital. 1976, 17, 1–60. (In Italian) [Google Scholar]
  60. Colonna, V.; Piccarretta, G. Schema strutturale della Sila Piccola Meridionale. Boll. Soc. Geol. Ital. 1975, 94, 3–16. (In Italian) [Google Scholar]
  61. Tursi, F.; Bianco, C.; Brogi, A.; Caggianelli, A.; Prosser, G.; Ruggieri, G.; Braschi, E. Cold subduction zone in northern Calabria (Italy) revealed by lawsonite–clinopyroxene blueschists. J. Metamorph. Geol. 2020, 38, 451–469. [Google Scholar] [CrossRef]
  62. Paglionico, A.; Piccarreta, G. History and petrology of a fragment of the deep crust in the Serre (Calabria, Italy). Neues. Jb. Miner. Monat. 1978, 9, 385–396. [Google Scholar]
  63. Rossetti, F.; Goffé, B.; Monié, P.; Faccenna, C.; Vignaroli, G. Alpine orogenic P-T-t-deformation history of the Catena Costiera area and surrounding regions (Calabrian Arc, southern Italy): The nappe edifice of north Calabria revised with insights on the Tyrrhenian-Apennine system formation. Tectonics 2004, 23, TC6011. [Google Scholar] [CrossRef]
  64. Liberi, F.; Morten, L.; Piluso, E. Geodynamic significance of ophiolites within the Calabrian Arc. Isl. Arc 2006, 15, 26–43. [Google Scholar] [CrossRef]
  65. Brandt, S.; Schenk, V. Metamorphic response to Alpine thrusting of a crustal-scale basement nappe in southern Calabria (Italy). J. Petrol. 2020, 61, egaa063. [Google Scholar] [CrossRef]
  66. Ortolano, G.; Visalli, R.; Fazio, E.; Fiannacca, P.; Godard, G.; Pezzino, A.; Punturo, R.; Sacco, V.; Cirrincione, R. Tectono-metamorphic evolution of the Calabria continental lower crust: The case of the Sila Piccola Massif. Int. J. Earth Sci. 2020, 109, 1295–1319. [Google Scholar] [CrossRef]
  67. Tursi, F.; Acquafredda, P.; Festa, V.; Fornelli, A.; Langone, A.; Micheletti, F.; Spiess, R. What can high-P sheared orthogneisses tell us? An example from the Curinga–Girifalco Line (Calabria, southern Italy). J. Metamorph. Geol. 2021, 39, 919–944. [Google Scholar] [CrossRef]
  68. Dubois, R. Définition d’un socle anté hercynien en Calabre. CR Acad. Sci. 1971, 272, 2052–2055. [Google Scholar]
  69. Schenk, V. The exposed crustal cross section of southern Calabria, Italy: Structure and evolution of a segment of Hercynian crust. In Exposed Cross-Sections of the Continental Crust; Salisbury, M.H., Fountain, D.M., Eds.; Springer: Dordrecht, The Netherlands, 1990; pp. 21–42. [Google Scholar]
  70. Graessner, T.; Schenk, V. An exposed Hercynian deep crustal section in the Sila Massif of northern Calabria: Mineral chemistry, petrology and a P–T path of granulite-facies metapelitic migmatites and metabasites. J. Petrol. 2001, 42, 931–961. [Google Scholar] [CrossRef] [Green Version]
  71. Festa, V.; Messina, A.; Paglionico, A.; Piccarreta, G.; Rottura, A. Pre-Triassic history recorded in the Calabria–Peloritani segment of the Alpine chain, southern Italy. An overview. Period. Mineral. 2004, 73, 57–71. [Google Scholar]
  72. Festa, V.; Cicala, M.; Tursi, F. The Curinga–Girifalco Line in the framework of the tectonic evolution of the remnant Alpine chain in Calabria (southern Italy). Int. J. Earth Sci. 2020, 109, 2583–2598. [Google Scholar] [CrossRef]
  73. Festa, V.; Caggianelli, A.; Kruhl, J.H.; Liotta, D.; Prosser, G.; Gueguen, E.; Paglionico, A. Late-Hercynian shearing during crystallization of granitoid magmas (Sila Massif, southern Italy): Regional implications. Geodin. Acta 2006, 19, 185–195. [Google Scholar] [CrossRef] [Green Version]
  74. Fornelli, A.; Festa, V.; Micheletti, F.; Spiess, R.; Tursi, F. Building an orogen: Review of U-Pb zircon ages from the Calabria–Peloritani terrane to constrain the timing of the southern Variscan belt. Minerals 2020, 10, 944. [Google Scholar] [CrossRef]
  75. Vignaroli, G.; Minelli, L.; Rossetti, F.; Balestrieri, M.L.; Faccenna, C. Miocene thrusting in the eastern Sila Massif: Implication for the evolution of the Calabria-Peloritani orogenic wedge (southern Italy). Tectonophysics 2012, 538, 105–119. [Google Scholar] [CrossRef]
  76. Cirrincione, R.; Fazio, E.; Fiannacca, P.; Pezzino, A.; Ortolano, G.; Punturo, R. The Calabria-Peloritani Orogen, a composite terrane in Central Mediterranean; its overall architecture and geodynamic significance for a pre-Alpine scenario around the Tethyan basin. Period. Mineral. 2015, 84, 701–749. [Google Scholar]
  77. Caggianelli, A.; Prosser, G.; Rottura, A. Thermal history vs. fabric anisotropy in granitoids emplaced at different crustal levels: An example from Calabria, Southern Italy. Terra Nova 2000, 12, 109–116. [Google Scholar] [CrossRef]
  78. Langone, A.; Caggianelli, A.; Festa, V.; Prosser, G. Time constraints on the building of the Serre Batholith: Consequences for the thermal evolution of the Hercynian continental crust exposed in Calabria (southern Italy). J. Geol. 2014, 122, 183–199. [Google Scholar] [CrossRef]
  79. Festa, V.; Fornelli, A.; Paglionico, A.; Pascazio, A.; Piccarreta, G.; Spiess, R. Asynchronous extension of the late-Hercynian crust in Calabria. Tectonophysics 2012, 518–521, 29–43. [Google Scholar] [CrossRef]
  80. Moresi, M.; Paglionico, A.; Piccarreta, G.; Rottura, A. The deep crust in Calabria (Polia-Copanello Unit): A comparison with the Ivrea-Verbano zone. Mem. Sci. Geol. 1979, 33, 233–242. [Google Scholar]
  81. Acquafredda, P.; Fornelli, A.; Paglionico, A.; Piccarreta, G. Petrological evidence for crustal thickening and extension in the Serre granulite terrane (Calabria, southern Italy). Geol. Mag. 2006, 143, 145–163. [Google Scholar] [CrossRef]
  82. Acquafredda, P.; Fornelli, A.; Piccarreta, G.; Pascazio, A. Multi-stage dehydration-decompression in the metagabbros from the lower crustal rocks of the Serre (Southern Calabria, Italy). Geol. Mag. 2008, 145, 397–411. [Google Scholar] [CrossRef]
  83. Festa, V.; Fornelli, A.; Micheletti, F.; Spiess, R.; Tursi, F. Ductile shearing and focussed rejuvenation: Records of High-P (eo-)Alpine metamorphism in the Variscan Lower Crust (Serre Massif, Calabria—Southern Italy). Geosciences 2022, 12, 212. [Google Scholar] [CrossRef]
  84. De Vivo, B.; Ayuso, R.A.; Belkin, H.E.; Lima, A.; Messina, A.; Russo, S.; Viscardi, A. Whole-rock geochemistry and fluid inclusions as exploration tools for mineral deposits assessment in the Serre batholith, Calabria, southern Italy. Eur. J. Mineral. 1992, 4, 1035–1051. [Google Scholar] [CrossRef] [Green Version]
  85. Ayuso, R.A.; Messina, A.; De Vivo, B.; Russo, S.; Woodruff, L.G.; Sutter, J.F.; Belkin, H.E. Geochemistry and argon thermochronology of the Variscan Sila Batholith, southern Italy: Source rocks and magma evolution. Contrib. Mineral. Petr. 1994, 117, 87–109. [Google Scholar] [CrossRef]
  86. Rottura, A.; Bargossi, G.M.; Caironi, V.; Del Moro, A.; Maccarrone, E.; Macera, P.; Paglionico, A.; Petrini, R.; Piccarreta, G.; Poli, G. Petrogenesis of contrasting Hercynian granitoids from the Calabrian Arc, southern Italy. Lithos 1990, 24, 97–119. [Google Scholar] [CrossRef]
  87. Caggianelli, A.; Moro, A.D.; Piccarreta, G. Petrology of basic and intermediate orogenic granitoids from the Sila Massif (Calabria, southern Italy). Geol. J. 1994, 29, 11–28. [Google Scholar] [CrossRef]
  88. Fornelli, A.; Caggianelli, A.; Del Moro, A.; Bargossi, G.M.; Paglionico, A.; Piccarreta, G.; Rottura, A. Petrology and evolution of the Central Serre granitoids (southern Calabria–Italy). Period. Mineral. 1994, 63, 53–70. [Google Scholar]
  89. Fiannacca, P.; Williams, I.S.; Cirrincione, R. Timing and mechanisms of sequential granitoid emplacement in collapsing orogens: Insights from SHRIMP zircon U-Pb geochronology of the Serre Batholith (Calabria, southern Italy). In Proceedings of the 8th Hutton Symposium on Granites and Related Rocks, Florianopolis, Brazil, 20–25 September 2015. [Google Scholar]
  90. Fiannacca, P.; Williams, I.S.; Cirrincione, R. Timescales and mechanisms of batholith construction: Constraints from zircon oxygen isotopes and geochronology of the late Variscan Serre Batholith (Calabria, southern Italy). Lithos 2017, 277, 302–314. [Google Scholar] [CrossRef]
  91. Fiannacca, P.; Russo, D.; Fazio, E.; Cirrincione, R.; Mamtani, M.A. Fabric analysis in upper crustal post-collisional granitoids from the Serre Batholith (Southern Italy): Results from microstructural and AMS investigations. Geosciences 2021, 11, 414. [Google Scholar] [CrossRef]
  92. Festa, V.; Caggianelli, A.; Langone, A.; Prosser, G. Time–space relationships among structural and metamorphic aureoles related to granite emplacement: A case study from the Serre Massif (southern Italy). Geol. Mag. 2013, 150, 441–454. [Google Scholar] [CrossRef]
  93. Festa, V.; Tursi, F.; Caggianelli, A.; Spiess, R. The tectono-magmatic setting of the Hercynian upper continental crust exposed in Calabria (Italy) as revealed by the 1:10,000 structural-geological map of the Levadio stream area. Ital. J. Geosci. 2018, 137, 165–174. [Google Scholar] [CrossRef]
  94. Liotta, D.; Festa, V.; Caggianelli, A.; Prosser, G.; Pascazio, A. Mid-crustal shear zone evolution in a syn-tectonic late Hercynian granitoid (Sila Massif, Calabria, southern Italy). Int. J. Earth Sci. 2004, 93, 400–413. [Google Scholar] [CrossRef]
  95. Festa, V. C-axis fabrics of quartz-ribbons during high-temperature deformation of syn-tectonic granitoids (Sila Massif, Calabria, Italy). Comptes Rendus Geosci. 2009, 341, 557–567. [Google Scholar] [CrossRef]
  96. Tursi, F.; Spiess, R.; Festa, V.; Fregola, R.A. Hercynian subduction-related processes within the metamorphic continental crust in Calabria (southern Italy). J. Metamorph. Geol. 2020, 38, 771–793. [Google Scholar] [CrossRef]
  97. Angì, G.; Cirrincione, R.; Fazio, E.; Fiannacca, P.; Ortolano, G.; Pezzino, A. Metamorphic evolution of preserved Hercynian crustal section in the Serre Massif (Calabria–Peloritani Orogen, southern Italy). Lithos 2010, 115, 237–262. [Google Scholar] [CrossRef]
  98. Langone, A.; Godard, G.; Prosser, G.; Caggianelli, A.; Rottura, A.; Tiepolo, M. P–T–t path of the Hercynian low-pressure rocks from the Mandatoriccio complex (Sila Massif, Calabria, Italy): New insights for crustal evolution. J. Metamorph. Geol. 2010, 28, 137–162. [Google Scholar] [CrossRef]
  99. Acquafredda, P.; Lorenzoni, S.; Zanettin-Lorenzoni, E. Palaeozoic sequences and evolution of the Calabrian-Peloritan Arc (Southern Italy). Terra Nova 1994, 6, 582–594. [Google Scholar] [CrossRef]
  100. Festa, V.; Langone, A.; Caggianelli, A.; Rottura, A. Dike magmatism in the Sila Grande (Calabria, southern Italy): Evidence of Pennsylvanian–Early Permian exhumation. Geosphere 2010, 6, 549–566. [Google Scholar] [CrossRef] [Green Version]
  101. Romano, V.; Cirrincione, R.; Fiannacca, P.; Lustrino, M.; Tranchina, A. Late-Hercynian post-collisional dyke magmatism in central Calabria (Serre Massif, southern Italy). Period. Mineral. 2011, 80, 489–515. [Google Scholar]
  102. Roda, C. Il calcare portlandiano a Dasycladacee di M. Mutolo (Reggio Calabria). Geol. Rom. 1965, 4, 259–290. (In Italian) [Google Scholar]
  103. Bonardi, G.; Messina, A.; Perrone, V.; Russo, S.; Zuppetta, A. L’Unita di Stilo nel settore meridionale dell’Arco Calabro-Peloritano. Boll. Soc. Geol. Ital. 1984, 103, 279–309. [Google Scholar]
  104. Innamorati, G.; Santantonio, M. Evidence for extended Hercynian basement and a preserved Jurassic basin-margin tract in Northern Calabria (Southern Italy): The Longobucco Basin. Sediment. Geol. 2018, 376, 147–163. [Google Scholar] [CrossRef]
  105. Brondi, A.; Ferretti, O.; Masperoni, L.; Anselmi, B.; Benvegnù, F. Prospezione mineralogica alluvionale applicata in Calabria alla ricerca di minerali di Torio e Zirconio. Ind. Miner. 1972, 23, 233–247. (In Italian) [Google Scholar]
  106. Buchanan, L.J.; De Vivo, B.; Kramer, A.K.; Lima, A. Fluid inclusion study of the Fiumarella barite deposit (Catanzaro—S. Italy). Miner. Depos. 1981, 16, 215–226. [Google Scholar] [CrossRef]
  107. De Vivo, B.; Ayuso, R.A.; Belkin, H.E.; Lima, A.; Messina, A.; Viscardi, A. Rock chemistry and fluid inclusion studies as exploration tools for ore deposits in the Sila batholith, southern Italy. J. Geochem. Explor. 1991, 40, 291–310. [Google Scholar] [CrossRef]
  108. Benvenuti, M.; Morelli, F.; Lattanzi, P.; Ruggieri, G.; Tanelli, G. Mineralogy, textures and mineral chemistry of Au-Ag veins at Rossano, Calabrian-Peloritan Arc (Calabria, Italy). Mem. Soc. Geol. Ital. 1994, 48, 731–735. [Google Scholar]
  109. Colonna, V.; Zanettin-Lorenzoni, E. Gli scisti cristallini della Sila Piccola: 2- I rapporti tra la formazione delle filladi e la formazione delle pietre verdi nella zona di Gimigliano. Mem. Soc. Geol. Ital. 1972, 2, 261–292. (In Italian) [Google Scholar]
  110. Cuteri, F.A. Paesaggi minerari in Calabria: L’Argentera di Longobucco (CS). In Proceedings of the “VI Congresso Nazionale di Archeologia Medievale”, L’Aquila, Italy, 12—15 September 2012; Redi, F., Forgione, A., Eds.; 2012; pp. 401–406. (In Italian). [Google Scholar]
  111. Arnoni, E. La Calabria Illustrata. Parte Seconda.; Tipografia Municipale: Cosenza, Italy, 1875. (In Italian) [Google Scholar]
  112. Omenetto, P.; Meggiolaro, V.; Spagna, P.; Brigo, L.; Ferla, P.; Guion, J.L. Scheelite-bearing metalliferous sequences of the Peloritani Mountains, Northeastern Sicily (with some remarks on Tungsten metallogenesis in the Calabrian-Peloritan Arc). In Mineral Deposits within the European Community; Boissonas, J., Omenetto, P., Eds.; Springer: Berlin/Heidelberg, Germany, 1988; pp. 179–198. [Google Scholar]
  113. Croze, V. Etude du Skarn à Tungstène de LONGOBUCCO (Calabre, Italie) dans son Environnement Granitique. Pétrographie et géOchimie. Ph.D. Thesis, Sciences de la Terre, Université Pierre et Marie Curie—Paris VI, Paris, France, 1989; p. 63. Available online: https://theses.hal.science/tel-01052928v1 (accessed on 17 March 2023). (In French).
  114. Burragato, F. Contributo alla conoscenza dei minerali uraniferi della Calabria. Period. Mineral. 1966, 35, 387–402. (In Italian) [Google Scholar]
  115. MICA. Relazione sul Servizio Minerario e Statistico Dell’Industria Estrattiva in Italia Negli Anni 1957–59; Ministero Commercio Industria e Artigianato, Corpo Statale delle Miniere: Roma, Italy, 1957. (In Italian) [Google Scholar]
  116. Dattola, L. La miniera di barite del Torrente Fiumarella presso Catanzaro: I minerali. Riv. Mineral. Ital. 1996, 20, 289–292. (In Italian) [Google Scholar]
  117. Bloise, A.; Dattola, L.; Allegretta, I.; Terzano, R.; Taranto, M.; Miriello, D. First evidence of wulfenite in Calabria region (Southern Italy). Data Brief 2018, 19, 687–692. [Google Scholar] [CrossRef] [PubMed]
  118. Bloise, A.; Dattola, L.; Allegretta, I.; Terzano, R.; Miriello, D. Linarite and connellite from Calabria region (Southern Italy): First evidence. Data Brief 2019, 27, 104597. [Google Scholar] [CrossRef]
  119. Scacchi, A. Granato di Tiriolo in Calabria. Rend. Lincei 1886, 2, 988–989. (In Italian) [Google Scholar]
  120. Fiumano, F. Lo spinello zincifero di Tiriolo (Catanzaro). Not. Mineral. Sicil. E Cal. 1947, 1, 55–59. (In Italian) [Google Scholar]
  121. Mauro, F. Analisi chimica dello spinello in Calabria. Atti Accad. Lincei trans. 1879, 3, 65–66. (In Italian) [Google Scholar]
  122. De Angelis, G.; Iocca, M.; Palmarelli, A. Nota sullo spinello azzurro di Tiriolo (Calabria). Period. Mineral. 1982, 51, 225–232. (In Italian) [Google Scholar]
  123. Lucchesi, S.; Della Giusta, A.; Russo, U. Cation distribution in natural Zn-aluminate spinels. Mineral. Mag. 1998, 62, 41–54. [Google Scholar] [CrossRef]
  124. Fregola, R.A.; Skogby, H.; Bosi, F.; D’Ippolito, V.; Andreozzi, G.B.; Hålenius, U. Optical absorption spectroscopy study of the causes for color variations in natural Fe-bearing gahnite: Insights from iron valency and site distribution data. Am. Mineral. 2014, 99, 2187–2195. [Google Scholar] [CrossRef]
  125. D’Ippolito, V.; Andreozzi, G.B.; Bosi, F.; Hålenius, U.; Mantovani, L.; Bersani, D.; Fregola, R.A. Crystallographic and spectroscopic characterization of a natural Zn-rich spinel approaching the endmember gahnite (ZnAl2O4) composition. Mineral. Mag. 2013, 77, 2941–2953. [Google Scholar] [CrossRef]
  126. Crisci, G.M.; Dattola, L. Minerali del Catanzarese e Crotonese. In Il Gabinetto di Storia Naturale del Liceo “P. Galluppi” di Catanzaro e la Geologia Della Calabria nell’800; Procopio, F., Marabini, S., Eds.; Centro Editoriale e Librario Università della Calabria: Cosenza, Italy, 2001; pp. 39–48. (In Italian) [Google Scholar]
  127. Spica, M. Intorno all’analisi di un minerale di molibdeno e sulla esistenza di un tetramolibdato ferroso. La Gazz. Chim. Ital. 1894, 24, 97–111. (In Italian) [Google Scholar]
  128. Carobbi, G. Sulla ferromolibdite di Bivongi (Calabria). Rend. Accad. Sci. Fis. Mat. (Cl. Soc. R. Napoli) 1927, 34, 53. (In Italian) [Google Scholar]
  129. Baldanza, B.; Triscari, M. Sulle mineralizzazioni a molibdeno della Calabria. Rend. Soc. Ital. Mineral. Petrol. 1979, 35, 455. (In Italian) [Google Scholar]
  130. Vighi, L. Su alcune aree calabresi segnalate quali sedi di manifestazioni metallifere. Ind. Miner. 1951, 2, 297–303. (In Italian) [Google Scholar]
  131. Vighi, L. Sulla genesi dei prodotti di alterazione della pirite in ganga di quarzo. Period. Mineral. 1951, 20, 1–42. (In Italian) [Google Scholar]
  132. Finger, F.; Roberts, M.P.; Haunschmid, B.; Schermaier, A.; Steyrer, H.P. Variscan granitoids of central Europe: Their typology, potential sources and tectonothermal relations. Miner. Petrol. 1997, 61, 67–96. [Google Scholar] [CrossRef]
  133. Wilson, M.; Neumann, E.R.; Davies, G.R.; Timmerman, M.J.; Heeremans, M.; Larsen, B.T. Permo-Carboniferous magmatism and rifting in Europe: Introduction. In Permo-Carboniferous Magmatism and Rifting in Europe; Wilson, M., Neumann, E.R., Davies, G.R., Timmerman, M.J., Heeremans, M., Larsen, B.T., Eds.; The Geological Society: London, UK, 2004; Volume 223, pp. 1–10. [Google Scholar]
  134. Marignac, C.; Cuney, M. Ore deposits of the French Massif Central: Insight into the metallogenesis of the Variscan collision belt. Miner. Depos. 1999, 34, 472–504. [Google Scholar] [CrossRef]
  135. Belissont, R.; Boiron, M.-C.; Luais, B.; Cathelineau, M. LA-ICP-MS analyses of minor and trace elements and bulk Ge isotopes in zoned Ge-rich sphalerites from the Noailhac—Saint-Salvy deposit (France): Insights into incorporation mechanisms and ore deposition processes. Geochim. Cosmochim. Acta 2014, 126, 518–540. [Google Scholar] [CrossRef]
  136. Alles, J.; Ploch, A.M.; Schirmer, T.; Nolte, N.; Liessmann, W.; Lehmann, B. Rare-earth-element enrichment in post-Variscan polymetallic vein systems of the Harz Mountains, Germany. Miner. Depos. 2019, 54, 307–328. [Google Scholar] [CrossRef]
  137. Bauer, M.E.; Burisch, M.; Ostendorf, J.; Krause, J.; Frenzel, M.; Seifert, T.; Gutzmer, J. Trace element geochemistry of sphalerite in contrasting hydrothermal fluid systems of the Freiberg district, Germany: Insights from LA-ICP-MS analysis, near-infrared light microthermometry of sphalerite-hosted fluid inclusions, and sulfur isotope geochemistry. Miner. Depos. 2019, 54, 237–262. [Google Scholar]
  138. Ostendorf, J.; Henjes-Kunst, F.; Seifert, T.; Gutzmer, J. Age and genesis of polymetallic veins in the Freiberg district, Erzgebirge, Germany: Constraints from radiogenic isotopes. Miner. Depos. 2019, 54, 217–236. [Google Scholar] [CrossRef]
  139. Swinkels, L.J.; Schulz-Isenbeck, J.; Frenzel, M.; Gutzmer, J.; Burisch, M. Spatial and temporal evolution of the Freiberg epithermal Ag-Pb-Zn district, Germany. Econ. Geol. 2021, 116, 1649–1667. [Google Scholar] [CrossRef]
  140. Pažout, R.; Sejkora, J.; Šrein, V. Ag-Pb-Sb sulfosalts and Se-rich mineralization of Anthony of Padua Mine near Poličany—Model example of the mineralization of Silver Lodes in the historic Kutná Hora Ag-Pb ore district, Czech Republic. Minerals 2019, 9, 430. [Google Scholar] [CrossRef] [Green Version]
  141. Boni, M.; Muchez, P.; Schneider, J. Permo-Mesozoic multiple fluid flow and ore deposits in Sardinia: A comparison with post-Variscan mineralization of Western Europe. In The Timing and Location of Major Ore Deposits in an Evolving Orogen; Blundell, D.J., Neubauer, F., von Quadt, A., Eds.; The Geological Society: London, UK, 2002; Volume 204, pp. 199–211. [Google Scholar]
  142. Naitza, S.; Conte, A.M.; Cuccuru, S.; Oggiano, G.; Secchi, F.; Tecce, F. A Late Variscan tin province associated to the ilmenite-series granites of the Sardinian Batholith (Italy): The Sn and Mo mineralisation around the Monte Linas ferroan granite. Ore Geol. Rev. 2017, 80, 1259–1278. [Google Scholar] [CrossRef]
  143. Moroni, M.; Naitza, S.; Ruggieri, G.; Aquino, A.; Costagliola, P.; De Giudici, G.; Caruso, S.; Ferrari, E.; Fiorentini, M.L.; Lattanzi, P. The Pb-Zn-Ag vein system at Montevecchio-Ingurtosu, southwestern Sardinia, Italy: A summary of previous knowledge and new mineralogical, fluid inclusion, and isotopic data. Ore Geol. Rev. 2019, 115, 103194. [Google Scholar] [CrossRef]
  144. Boni, M.; Balassone, G.; Fedele, L.; Mondillo, N. Post-Variscan hydrothermal activity and ore deposits in southern Sardinia (Italy): Selected examples from Gerrei (Silius Vein System) and the Iglesiente district. Period. Mineral. 2009, 78, 19–35. [Google Scholar]
  145. Höll, R.; Kling, M.; Schrol, E. Metallogenesis of germanium—A review. Ore Geol. Rev. 2007, 30, 145–180. [Google Scholar] [CrossRef]
  146. Halfon, J.; Rosique, A. Comparaison des éléments «en trace » dans les blendes du filon et du stratiforme de Saint-Salvy (Tarn). Bull. Bur. Rech. Géol. Min. 1973, 5, 403–432. [Google Scholar]
Minerals 13 00439 g001 550
Figure 1. Geographic sketch-map of Calabria with toponyms of the areas characterized by mineralization.
Figure 1. Geographic sketch-map of Calabria with toponyms of the areas characterized by mineralization.
Minerals 13 00439 g001
Minerals 13 00439 g002 550
Figure 2. (a) Sketch map showing the distribution of basement rocks exposed in Southern Italy (modified after [71]); (b) sketch map of the lower, middle, and upper late-Variscan continental crust exposed in Calabria (modified after [68]); (c) geological sketch-map of the Sila Massif area with numbered location (numbers 1–20 in the white circles are the same as reported in Table A1 and in paragraph 4) of the pertaining mineralization sites (modified after [73,74,75,76]). 1—Ophiolite units (e.g., Gimigliano and Diamante-Terranova units). 2—Fiume Pomo Unit (former Bagni-Fondachelli Unit; dominant phyllites). 3—Castagna Unit (dominant augen gneisses). Sila-Serre Unit: 4—former Monte Gariglione and Polia-Copanello units (granulites, gneisses, paragneisses, migmatites); 5, 6, 7a–c—Sila and Serre batholiths (i.e., 5—norite-diorite; 6—tonalites; 7a—granodiorite; 7b—Bt-Ms cordierite-bearing granodiorite-monzogranite; 7c—Bt-Ms-And-Sil-Crd-bearing granodiorite-monzogranite, Bt-Ms-And-Sil-Crd leucogranite, and small fine-grained granite); 8a—Mandatoriccio/Mammola Unit (dominant schists); 8b—contact aureole (spotted schists and fels at the expense of the Mandatoriccio/Mammola Unit schists); 9a—Bocchigliero/Stilo-Pazzano Unit (dominant phyllites); 9b—contact aureole (spotted schists and fels at the expense of the Bocchigliero/Stilo-Pazzano Unit phyllites); 10—Longobucco/Stilo cover (dominant carbonates). Main Alpine thrust at the base of the: 11—Sila-Serre Unit; 12—Castagna Unit; 13—Fiume Pomo Unit. 14 –Minor Alpine thrust and faults. 15—Hercynian shear zone. 16—Lithostratigraphic contact.
Figure 2. (a) Sketch map showing the distribution of basement rocks exposed in Southern Italy (modified after [71]); (b) sketch map of the lower, middle, and upper late-Variscan continental crust exposed in Calabria (modified after [68]); (c) geological sketch-map of the Sila Massif area with numbered location (numbers 1–20 in the white circles are the same as reported in Table A1 and in paragraph 4) of the pertaining mineralization sites (modified after [73,74,75,76]). 1—Ophiolite units (e.g., Gimigliano and Diamante-Terranova units). 2—Fiume Pomo Unit (former Bagni-Fondachelli Unit; dominant phyllites). 3—Castagna Unit (dominant augen gneisses). Sila-Serre Unit: 4—former Monte Gariglione and Polia-Copanello units (granulites, gneisses, paragneisses, migmatites); 5, 6, 7a–c—Sila and Serre batholiths (i.e., 5—norite-diorite; 6—tonalites; 7a—granodiorite; 7b—Bt-Ms cordierite-bearing granodiorite-monzogranite; 7c—Bt-Ms-And-Sil-Crd-bearing granodiorite-monzogranite, Bt-Ms-And-Sil-Crd leucogranite, and small fine-grained granite); 8a—Mandatoriccio/Mammola Unit (dominant schists); 8b—contact aureole (spotted schists and fels at the expense of the Mandatoriccio/Mammola Unit schists); 9a—Bocchigliero/Stilo-Pazzano Unit (dominant phyllites); 9b—contact aureole (spotted schists and fels at the expense of the Bocchigliero/Stilo-Pazzano Unit phyllites); 10—Longobucco/Stilo cover (dominant carbonates). Main Alpine thrust at the base of the: 11—Sila-Serre Unit; 12—Castagna Unit; 13—Fiume Pomo Unit. 14 –Minor Alpine thrust and faults. 15—Hercynian shear zone. 16—Lithostratigraphic contact.
Minerals 13 00439 g002
Minerals 13 00439 g003 550
Figure 3. Geological sketch-map of the Serre Massif area with numbered location (numbers 21–28 in the white circles are the same as reported in Table A2 and in paragraph 5) of the pertaining mineralization sites (modified after [74,76]). 1—Fiume Pomo Unit (former Bagni-Fondachelli Unit; dominant phyllites). 2—Castagna Unit (dominant augen gneisses). Sila-Serre Unit: 3—former Monte Gariglione/Polia-Copanello Unit (i.e., 3a—felsic and mafic granulites; metapelites and metagabbros; 3b—migmatitic metapelites; 3c—migmatitic border zone); 4, 5a,b—Sila and Serre batholiths (i.e., 4—tonalites; 5a—granodiorite; 5b—Bt-Ms cordierite-bearing granodiorite-monzogranite); 6a—Mandatoriccio/Mammola Unit (dominant schists); 6b—contact aureole (spotted schists and fels at the expense of the Mandatoriccio/Mammola Unit schists); 7a—Bocchigliero/Stilo-Pazzano Unit (dominant phyllites); 7b—contact aureole (spotted schists and fels at the expense of the Bocchigliero/Stilo-Pazzano Unit phyllites). 8—Longobucco/Stilo cover (dominant carbonates). Main Alpine thrust at the base of the: 9—Sila-Serre Unit; 10—Castagna Unit. 11—Hercynian shear zone. 12—Lithostratigraphic contact.
Figure 3. Geological sketch-map of the Serre Massif area with numbered location (numbers 21–28 in the white circles are the same as reported in Table A2 and in paragraph 5) of the pertaining mineralization sites (modified after [74,76]). 1—Fiume Pomo Unit (former Bagni-Fondachelli Unit; dominant phyllites). 2—Castagna Unit (dominant augen gneisses). Sila-Serre Unit: 3—former Monte Gariglione/Polia-Copanello Unit (i.e., 3a—felsic and mafic granulites; metapelites and metagabbros; 3b—migmatitic metapelites; 3c—migmatitic border zone); 4, 5a,b—Sila and Serre batholiths (i.e., 4—tonalites; 5a—granodiorite; 5b—Bt-Ms cordierite-bearing granodiorite-monzogranite); 6a—Mandatoriccio/Mammola Unit (dominant schists); 6b—contact aureole (spotted schists and fels at the expense of the Mandatoriccio/Mammola Unit schists); 7a—Bocchigliero/Stilo-Pazzano Unit (dominant phyllites); 7b—contact aureole (spotted schists and fels at the expense of the Bocchigliero/Stilo-Pazzano Unit phyllites). 8—Longobucco/Stilo cover (dominant carbonates). Main Alpine thrust at the base of the: 9—Sila-Serre Unit; 10—Castagna Unit. 11—Hercynian shear zone. 12—Lithostratigraphic contact.
Minerals 13 00439 g003
Minerals 13 00439 g004 550
Figure 4. Schematic stratigraphic columns of the Sila-Serre Unit, in the Sila (a) and Serre (b) areas (modified after [71]), with numbered location of pertaining mineralization sites (numbers 1–28 in the squares are the same as reported in Table A1 and Table A2, and in paragraphs 4 and 5) framed in the different structural levels; the Alpine Castagna, Fiume Pomo and Ophiolite units are also reported. 1—Longobucco/Stilo cover. 2—Peraluminous granites. 3—Granodiorites and granites. 4—K-feldspar megacryst-bearing granodiorites. 5—Quartz-diorites to tonalites. 6—Slates, phyllites with interbedded (a) marbles and (b) metavolcanites of the Bocchigliero and Stilo-Pazzano units, derived from Cambrian to Carboniferous protoliths (dots indicate the metamorphic contact aureole). 7—Micaschists of the Mandatoriccio and Mammola units (dots indicate the metamorphic contact aureole). 8—Migmatitic border zone. 9—Migmatitic paragneisses with interbedded (a) marbles and (b) metabasites. 10—Felsic granulites. 11—Layered metagabbroic rocks. 12—Castagna Unit. 13—Fiume Pomo Unit. 14—Ophiolite units. 15—Alpine tectonic contacts (line colors as in Figure 2 and Figure 3).
Figure 4. Schematic stratigraphic columns of the Sila-Serre Unit, in the Sila (a) and Serre (b) areas (modified after [71]), with numbered location of pertaining mineralization sites (numbers 1–28 in the squares are the same as reported in Table A1 and Table A2, and in paragraphs 4 and 5) framed in the different structural levels; the Alpine Castagna, Fiume Pomo and Ophiolite units are also reported. 1—Longobucco/Stilo cover. 2—Peraluminous granites. 3—Granodiorites and granites. 4—K-feldspar megacryst-bearing granodiorites. 5—Quartz-diorites to tonalites. 6—Slates, phyllites with interbedded (a) marbles and (b) metavolcanites of the Bocchigliero and Stilo-Pazzano units, derived from Cambrian to Carboniferous protoliths (dots indicate the metamorphic contact aureole). 7—Micaschists of the Mandatoriccio and Mammola units (dots indicate the metamorphic contact aureole). 8—Migmatitic border zone. 9—Migmatitic paragneisses with interbedded (a) marbles and (b) metabasites. 10—Felsic granulites. 11—Layered metagabbroic rocks. 12—Castagna Unit. 13—Fiume Pomo Unit. 14—Ophiolite units. 15—Alpine tectonic contacts (line colors as in Figure 2 and Figure 3).
Minerals 13 00439 g004
Disclaimer/Publisher’s Note: The statements, opinions and data contained in all publications are solely those of the individual author(s) and contributor(s) and not of MDPI and/or the editor(s). MDPI and/or the editor(s) disclaim responsibility for any injury to people or property resulting from any ideas, methods, instructions or products referred to in the content.

Share and Cite

MDPI and ACS Style

Fregola, R.A.; Ciccolella, A.; Festa, V.; Ruggieri, G.; Schingaro, E.; Tursi, F.; Ventruti, G. Review of Polymetallic Mineralization in the Sila and Serre Massifs (Calabria, Southern Italy). Minerals 2023, 13, 439. https://doi.org/10.3390/min13030439

AMA Style

Fregola RA, Ciccolella A, Festa V, Ruggieri G, Schingaro E, Tursi F, Ventruti G. Review of Polymetallic Mineralization in the Sila and Serre Massifs (Calabria, Southern Italy). Minerals. 2023; 13(3):439. https://doi.org/10.3390/min13030439

Chicago/Turabian Style

Fregola, Rosa Anna, Antonio Ciccolella, Vincenzo Festa, Giovanni Ruggieri, Emanuela Schingaro, Fabrizio Tursi, and Gennaro Ventruti. 2023. "Review of Polymetallic Mineralization in the Sila and Serre Massifs (Calabria, Southern Italy)" Minerals 13, no. 3: 439. https://doi.org/10.3390/min13030439

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop