Formation and Characteristics of Sediment-Hosted Ore Deposits

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

Deadline for manuscript submissions: 27 February 2026 | Viewed by 51

Special Issue Editors


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Guest Editor
School of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China
Interests: micro-fabrics; paleo-stress field in ore deposits

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Guest Editor
School of the Environment, University of Queensland, Brisbane, QLD 4072, Australia
Interests: sedimentary geochemistry; diagenesis; basin analysis

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Guest Editor
School of Biological, Earth & Environmental Sciences, University of New South Wales, Sydney, NSW 2052, Australia
Interests: trace element geochemistry; ore deposit formation

Special Issue Information

Dear Colleagues,

Research on sediment-hosted ore deposits is a global endeavor. Driven by increasing demand for copper, gold, and uranium, new deposits continue to be discovered annually. These sediment-hosted ore deposits, which may or may not originate from sedimentary processes, arise from a diversity of geological mechanisms, including hydrothermal or magmatic sources within layer-parallel shear zones.

This Special Issue is a testament to the power of interdisciplinary collaboration, presenting the latest advances in the study of sediment-hosted ore deposits. By combining the expertise of various fields—including mineralogy, petrology, structural geology, geochemistry, geochronology, geomorphology, and regional tectonics—we aim to unlock crucial insights into the formation and deformation mechanisms that create sediment-hosted ore deposits. This interdisciplinary approach enables a comparative analysis of temporal and geographic patterns in ore deposit formation on a global scale.

We invite submissions that include original scientific research relating to sediment-hosted deposits from established and newly identified localities worldwide. The Special Issue focuses on the following topics:

  • The geological background, occurrence, and genesis of sediment-hosted deposits;
  • The mineralogical, geochemical, spectroscopic, and microstructural characteristics of stratum layers;
  • Integrated methodologies for examining the provenance of sediment-hosted deposits as well as deposit identification and vectoring.

Dr. Hongyuan Zhang
Dr. William Defliese
Dr. Indrani Mukherjee
Guest Editors

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

  • formation
  • deformation
  • ore deposits
  • characteristics
  • stress field
  • mineralization
  • sediment-hosted

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Published Papers

This special issue is now open for submission.
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