Special Issue "Mineral, Fluid, and Melt Inclusions—Analysis, Interpretation, and Application, Volume II"

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

Deadline for manuscript submissions: 30 June 2023 | Viewed by 716

Special Issue Editor

School of the Environment, University of Windsor, Windsor, ON N9B 3P4, Canada
Interests: geochemistry; hydrothermal mineral deposits; laser ablation ICP-MS
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Mineral, fluid, and melt inclusions provide critical information on the physicochemical properties of geochemical systems that are unobtainable by other means. Combining inclusion petrography, compositional information, phase equilibria, and modeling gives unique insights into geologic spaces, times, and processes that are otherwise inaccessible and significantly contributes to advancement in diverse areas including petrology, mineral deposits, and hydrocarbon reservoir characterization, among others. This Special Issue, the second of its kind, will combine the latest advances in mineral, fluid, and melt inclusion analysis and interpretation with studies in the application of inclusions to a spectrum of geologic environments and investigations. Consequently, submissions spanning the breadth and depth of mineral, fluid, and melt inclusion science are encouraged.

Dr. Joel E. Gagnon
Guest Editor

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Minerals is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2000 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • mineral, fluid, and melt inclusions
  • geofluids
  • microthermometric analysis
  • elemental, isotopic, and molecular microanalysis
  • bulk analysis
  • inclusion synthesis
  • thermodynamics and modeling
  • mineral deposits
  • petrology
  • hydrocarbon reservoirs

Related Special Issue

Published Papers (1 paper)

Order results
Result details
Select all
Export citation of selected articles as:

Research

Article
Formation of High-Silica Leucocratic Granitoids on the Late Devonian Peraluminous Series of the Russian Altai: Mineralogical, Geochemical, and Isotope Reconstructions
Minerals 2023, 13(4), 496; https://doi.org/10.3390/min13040496 - 31 Mar 2023
Viewed by 506
Abstract
This paper presents data on the geological position, geochemical features, main mineral composition (micas, feldspars), and melt and fluid inclusions in quartz from Aba high-silica leucocratic granitoids in the western part of the Talitsa batholith, Russian Altai. According to these new geochemical data, [...] Read more.
This paper presents data on the geological position, geochemical features, main mineral composition (micas, feldspars), and melt and fluid inclusions in quartz from Aba high-silica leucocratic granitoids in the western part of the Talitsa batholith, Russian Altai. According to these new geochemical data, the granitoids are classified as S-type, meaning they are formed via the partial melting of metasedimentary source rocks. Geological data and oxygen isotope composition analysis indicate that major-phase granitoid magma evolution took place at the level of intrusion formation, whereas the parent melt of late-phase leucogranite evolved in a deeper chamber. The geochemical features (HFSE and REE, and REE spectra) of the granitoids indicate significantly higher differentiation in the late leucocratic phase. The presence of coexisting syngenetic melt and fluid inclusions shows that leucogranite magma was already saturated with volatiles in the early crystallization stages. Based on the new data presented in this work, the Aba rock formation is associated with the volatile saturation of magmatic melts, the exsolution of a fluid phase, and magma degassing. Full article
Show Figures

Figure 1

Back to TopTop