Special Issue "Petrogenesis, Magmatism and Geodynamics of Orogenic Belts"

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Geochemistry and Geochronology".

Deadline for manuscript submissions: 20 October 2023 | Viewed by 1700

Special Issue Editors

College of Earth Science, Chengdu University of Technology, Chengdu 610059, China
Interests: magmatism and tectonic evolution in orogenic belt; Paleo-Tethyan orogeny; crust–mantle interaction
Special Issues, Collections and Topics in MDPI journals
School of Geosciences, Yangtze University, Wuhan 430100, China
Interests: igneous petrology and geochemistry; paleo-tethyan tectono-magmatic evolution; magmatism and petroleum exploration

Special Issue Information

Dear Colleagues,

The formation of igneous rocks in orogenic belts is the response to the coupling of the crust–mantle material cycle and geodynamics. These structures represent important probes for revealing the growth mechanism of continental crust and associated deep geodynamic processes. Igneous rocks, generated in different tectonic settings including the opening and closing of oceanic basin, terranes collision and post-collisional extension, usually exhibit different rock assemblages and geochemical compositions, thus making them the key objects for tectonic reconstruction. The fact that magma sources and evolution processes play key roles in their origin is well known, however, how and to what degree do the different magma sources and magmatic evolution processes contribute to the petrological and geochemical diversity of igneous rocks in orogenic belts is debated and remains controversial. Over the past few decades, the scientific community has made a variety of breathroghs in their understanding of magma reservoirs. Unlike the conceptual melt-dominated magma chamber model, numerous geophysical and petrological studies have revealed that magma chambers mostly exist in the form of crystal-rich mush reservoirs. This new model requires us to rethink and study the evolution process and petrogenesis of igneous rocks, especially the mechanism of crust–mantle interaction in crystal mush magma. Hence, Minerals is placing an open call for original research, methods, comprehensive summary and review papers and other types of submissions for a thematic Special Issue entitled “Petrogenesis, Magmatism and the Geodynamics of Orogenic Belts”. We particularly encourage (but are not limited to) contributions of the following issues:

  • Magma sources and petrological diversity;
  • Magmatic processes in crustal magma reservoir;
  • Magmatic tempos in orogenic belts and their implications for crust growth;
  • Mafic magmatism in different geodynamic processes;
  • Numerical modelling approaches predicting the magmatic evolution and geochemical diversity.

Dr. Fuhao Xiong
Dr. Bin Liu
Guest Editors

Manuscript Submission Information

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Keywords

  • magmatism
  • petrogenesis
  • magmatic process
  • magmatic reservoir
  • geodynamic
  • tectonic

Published Papers (2 papers)

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Research

Article
Petrogenesis and Geodynamic Significance of the Early Triassic Nanpo Adakitic Pluton of the Luang Prabang-Loei Tectonic Belt (Northwestern Laos) in the East Tethys Domain: Constraints from Zircon U-Pb-Hf Isotope Analyses and Whole-Rock Geochemistry
Minerals 2023, 13(6), 821; https://doi.org/10.3390/min13060821 - 16 Jun 2023
Cited by 1 | Viewed by 618
Abstract
Adakites are magmatic rocks with specific geochemical characteristics and specific dynamics that provide important clues to understanding the magmatic-tectonic evolution of orogenic belts. We studied the Early Triassic Nanpo adakitic pluton of the Luang Prabang-Loei tectonic belt in the Eastern Tethys domain (Laos [...] Read more.
Adakites are magmatic rocks with specific geochemical characteristics and specific dynamics that provide important clues to understanding the magmatic-tectonic evolution of orogenic belts. We studied the Early Triassic Nanpo adakitic pluton of the Luang Prabang-Loei tectonic belt in the Eastern Tethys domain (Laos Sarakan) using detailed petrological, zircon U-Pb chronological, whole-rock geochemical, and zircon Lu-Hf isotope studies to constrain their petrogenesis. The rocks are predominantly diorites and granodiorites with Early Triassic zircon U-Pb emplacement ages ranging from 247.9 ± 1.0 to 249.0 ± 2.4 Ma. Moderate SiO2 (56.26–65.95 wt%) and Na2O (3.24–5.00 wt%) contents, with Na2O/K2O values between 1.76 and 2.51 and A/CNK values between 0.81 and 0.94, indicate that the rocks belong to the metaluminous calc-alkaline rock series. The high Sr content (590–918 ppm), low Y (6.30–11.89 ppm) and Yb (1.99–3.44 ppm) contents, intermediate Mg# (42–50) values, and high Sr/Y and (La/Yb) N ratios (Sr/Y = 24–41, (La/Yb) N = 6.84–13.8) are typical for adakites. Zircon Hf isotope analysis shows a significant variation in the εHf(t) values (6.7–12.0), with a mean value of 9.4 and a TDM2 of 512–845 Ma. Geochemical evidence indicates that the Nanpo adakitic rock was formed by the partial melting of the thickened lower crust in the plate-breaking environment and has an important contribution to the underplated mantle-derived magma. We propose that the Early Triassic adakites in the Luang Prabang-Loei tectonic belt formed during the transition from subduction to a continental collision, and the mixing of crust- and mantle-derived magmas is the main mechanism for the growth of continental crust in the Paleo-Tethys orogenic belt of southeastern Asia. Full article
(This article belongs to the Special Issue Petrogenesis, Magmatism and Geodynamics of Orogenic Belts)
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Article
Late Ordovician High Ba-Sr Intrusion in the Eastern North Qilian Orogen: Implications for Crust–Mantle Interaction and Proto-Tethys Ocean Evolution
Minerals 2023, 13(6), 744; https://doi.org/10.3390/min13060744 - 30 May 2023
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Abstract
High Ba-Sr granitic rocks are widespread in Phanerozoic orogenic systems, and their petrogenesis is important for revealing the evolutionary process of the Proto-Tethys Ocean in the North Qilian orogenic belt. This paper presents a combination of zircon U-Pb age, whole-rock major and trace [...] Read more.
High Ba-Sr granitic rocks are widespread in Phanerozoic orogenic systems, and their petrogenesis is important for revealing the evolutionary process of the Proto-Tethys Ocean in the North Qilian orogenic belt. This paper presents a combination of zircon U-Pb age, whole-rock major and trace element concentrations, and Sr-Nd-Hf isotopic data for Caowa high Ba-Sr dioritic intrusion from the eastern part of the North Qilian orogenic belt, aiming to decipher its petrogenesis and tectonic setting. LA-ICP-MS zircon U-Pb dating yield an emplacement age of 450 ± 2 Ma for the Caowa intrusion, indicating a magmatic activity of the Late Ordovician. The Caowa quartz diorites contain moderate contents of SiO2, MgO, Mg#, and resultant high concentrations of Na2O + K2O, Fe2O3T, and Al2O3, displaying calc-alkaline and metaluminous characteristics. The studied samples have relatively elevated Ba (up to 1165 ppm) and Sr (561 to 646 ppm) contents, with obvious enrichment in LILEs (e.g., Ba, Th, U) and depletions in HFSEs (e.g., Nb, Ta, Ti), resembling those of typical high Ba-Sr granitoids in subduction zones. Together with enriched Sr-Nd isotopic composition [(87Sr/86Sr)i = 0.7082–0.7086, εNd(t) = −5.1 to −4.9], and the wide ranges of zircon εHf(t) values (−13.2 to +8.5), it suggests that these high Ba-Sr quartz diorites were derived from a mixture magma source between the ancient crust materials and the enriched lithospheric mantle metasomatized by fluid released from subducted oceanic crust or sediment. Taking into account the ophiolites, high pressure metamorphic rocks, and arc magmatic rocks in the region, we infer that due to the influence of the northward subduction of the Qilian Proto-Tethys Ocean, the Laohushan oceanic crust of the North Qilian back-arc basin was subducted during the Late Ordovician and resulted in extensive metasomatism of lithospheric mantle by fluids derived from oceanic crust or sediments, and the Caowa high Ba-Sr quartz diorites were generated in the process of crust–mantle interaction during the Late Ordovician. Full article
(This article belongs to the Special Issue Petrogenesis, Magmatism and Geodynamics of Orogenic Belts)
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