Sulphide Mineral Microstructure

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Crystallography and Physical Chemistry of Minerals & Nanominerals".

Deadline for manuscript submissions: closed (20 August 2021) | Viewed by 273

Special Issue Editor


E-Mail Website
Guest Editor
Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool L69 3GP, UK
Interests: sulphide mineral microstructure applied to understanding: how sulphide minerals self-organise; deformation mechanisms; mineral deposit history; fault movement history; localisation of gold (much of this work has made extensive use of EBSD, which has also been applied to silicate mineral microstructural problems); geopolymer concrete; pedagogy

Special Issue Information

Dear Colleagues,

Sulphide minerals are commonly studied in mineral deposits. However, they are ubiquitous in all types of rocks, though often ignored because most are opaque and typically constitute minor components. This Special Issue of Minerals seeks to raise awareness of the utility of sulphide minerals by bringing together new and novel research studies of sulphide mineral microstructure from across all areas of geoscience, such as:

  • Primary deposition of sulphide minerals (e.g., sedimentary deposition vs. in situ precipitation for formation of primary layering structure in hydrothermal and igneous systems; self-organisation in framboid, colloform, spherule structures);
  • Sulphide mineral deformation and recrystallisation (e.g., use of pyrite microstructures to determine PT path segments in metamorphosed mineral deposits and faults);
  • Integration of microstructure and microchemistry (e.g., the role of sulphide mineral deformation and recrystallisation in mobilising and concentrating critical metals; controls on sulphide mineral oxidation relevant to acid mine drainage, concrete damage).

Studies can be from across the breadth of geological settings—sedimentary, igneous, metamorphic, tectonics, environment—with the common theme being the importance of sulphide mineral microstructure in advancing understanding of the problem being addressed. Studies combining microstructural and microchemical analysis are particularly welcome.

Dr. Alan P. Boyle
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 2400 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

  • sulphide minerals
  • microstructure
  • microchemistry
  • deformation
  • recrystallisation
  • EBSD
  • diffusion pathways
  • self-organisation
  • critical metal enrichment
  • oxidation
  • environmental impact

Published Papers

There is no accepted submissions to this special issue at this moment.
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