Tectonic Setting and Provenance of Sedimentary Rocks

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

Deadline for manuscript submissions: 30 November 2025 | Viewed by 52

Special Issue Editors


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Guest Editor
Estación Regional del Noroeste, Instituto de Geología, Universidad Nacional Autónoma de México, Hermosillo, Sonora, Mexico
Interests: sedimentary geochemistry; clay mineralogy; stable isotopes; U-Pb geochronology; oceanic anoxic enviroments (OAEs); paleogeography; paleoceanography; provenance and paleoclimatic studies

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Guest Editor
Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Mexico City, Mexico
Interests: mineralogy; sedimentology; marine sediments; geochemistry; mineral chemistry; tectonics; surface features; and granulometry
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Special Issue Information

Dear Colleagues,

Clastic sedimentary rocks are produced through the physical disintegration of pre-excisting rocks during weathering and mechanical erosion. Clastic sedimentary rocks are significant because they are considerably useful for understanding Earth's evolution, paleogeography, and depositional environments. Clastic rocks mainly contain silicate minerals like quartz but also contain non-silicate minerals, including carbonates, sulfates, sulfides, oxides, and halides. Metalliferous deposits hosted by sedimentary rocks are typically associated with rift-related thick basinal volcano-sedimentary or sedimentary sequences.

Various methods are utilized to understand the sequence stratigraphy, biostratigraphy, paleoclimate, source rock characteristics, tectonic setting, and depositional environment of a sedimentary basin. In particular, petrography, geochemistry, and geochronology play a vital role in inferring the source rock characteristics and tectonic settings of sedimentary basins.

The geochemical composition of sedimentary rocks is widely used as a proxy to portray the nature of source rocks, as well as the tectonic setting and evolution of continental crust. Furthermore, the composition of sedimentary rocks enables us to better understand the processes that produce economic concentrations of minerals, whether formed via hydrothermal, magmatic, or metamorphic processes, or even a combination of these processes. Geochemical studies significantly contribute to mineral exploration programs at the regional reconnaissance scale.

In addition, chemostratigraphic techniques that utilize geochemical variations for stratigraphic correlation allow for better discrimination of rock species. In previous studies the utilization of chemostratigraphic concepts to understand the provenance signatures  of clastic sediments are not often used. This Special Issue will bring together new studies focusing on chemostratigraphy to correlate sedimentary sequences at the regional scale.

The purpose of this special issue on “Tectonic Setting and Provenance of Sedimentary Rocks” therefore is to better understand basin architecture and the depositional environment of sedimentary basins based on the geochemical and mineralogical composition of clastic sedimentary rocks.

This Special Issue addresses the following themes:

  1. Application of geochemistry in minerals and sedimentary ore deposits.
  2. Composition of sedimentary rocks, provenance, and tectonic setting.
  3. Geochemistry and geochronology of sedimentary rocks.
  4. Cheomostratigraphy and chronostratigraphy.
  5. Paleoweathering and paleoclimate.
  6. Usefulness of geochemistry in understanding depositional environments.
  7. Petrography and mineralogy of sedimentary rocks.

Dr. Jayagopal Madhavaraju
Dr. John S. Armstrong-Altrin
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

  • tectonic setting
  • provenance
  • chemostratigraphy
  • geochemistry
  • geochronology
  • sedimentary rocks

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