Sedimentary Basin Evolution: Tectonics, Sedimentation and Architecture

A special issue of Geosciences (ISSN 2076-3263). This special issue belongs to the section "Sedimentology, Stratigraphy and Palaeontology".

Deadline for manuscript submissions: 30 August 2026 | Viewed by 783

Special Issue Editor


E-Mail Website
Guest Editor
Department of Geology, Paleontology and Fossil Fuels, Sofia University “St. Kliment Ohridski”, 15 Tzar Osvoboditel Bd., 1504 Sofia, Bulgaria
Interests: regional geology; tectonics; geochemistry; geochronology

Special Issue Information

Dear Colleagues,

The interplay between tectonics and sedimentation dramatically affects the evolution of sedimentary basins that comprise the Earth's upper crust and shape its surface. These basins form in various tectonic settings, present amazing past surface landscapes through geological history, and record the dynamic processes that have modelled the basin architecture. Understanding the tectonic setting of sedimentary basins, involved sources, and provenance of sedimentary fill is of fundamental importance to reconstructing sedimentary environments and their links to paleogeography, subsequent orogenic build-up, and bulk evolution.

Recent advances in sedimentary petrology and geochemistry have provided critical insights for interpreting tectonic settings, revealing distinct paleoconditions of source regions, while analyzing fossil content and facies variations has helped improved our understanding of the relationships among stratigraphic units within sedimentary basins. Furthermore, the application of geochronologic techniques has contributed to unravelling the timing of depositional history in basin fills.

This Special Issue looks to compile multidisciplinary research investigating the complex inter-relationships between tectonics, sedimentation, sedimentary sources and their provenance, and basin architecture. We encourage contributions from all geoscience research fields that explore the interaction of sedimentary-basin-related processes across distinct geological settings and time scales. We also invite contributions on sedimentary processes and tectonic architectures of sedimentary basins that have impacts on natural resources, geohazards, and risks.

This Special Issue will focus on the following key themes and beyond:

  • Tectonic settings and tectonic control of sedimentary basin formation.
  • Paleontology, stratigraphy, and facies of basin sedimentary fill.
  • Geochemistry of sedimentary/metasedimentary rocks, their sources, and their provenance.
  • Depositional history through geological time derived from geochronology.
  • Modelling of sedimentary basins.
  • Implications of basin architecture on natural resources, geohazards, and risks.

Dr. Nikolay Bonev
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 250 words) can be sent to the Editorial Office for assessment.

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. Geosciences 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 1800 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

  • sedimentary rocks
  • stratigraphy
  • tectonics
  • geochronology
  • geochemistry
  • basin architecture
  • basin evolution

Benefits of Publishing in a Special Issue

  • Ease of navigation: Grouping papers by topic helps scholars navigate broad scope journals more efficiently.
  • Greater discoverability: Special Issues support the reach and impact of scientific research. Articles in Special Issues are more discoverable and cited more frequently.
  • Expansion of research network: Special Issues facilitate connections among authors, fostering scientific collaborations.
  • External promotion: Articles in Special Issues are often promoted through the journal's social media, increasing their visibility.
  • Reprint: MDPI Books provides the opportunity to republish successful Special Issues in book format, both online and in print.

Further information on MDPI's Special Issue policies can be found here.

Published Papers (1 paper)

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

Research

22 pages, 17254 KB  
Article
Late Paleozoic and Late Jurassic Sedimentation at the Eurasian Continental Margin: Further Constraints from the Metasedimentary Successions of the Circum-Rhodope Belt, Greece
by Nikolay Bonev
Geosciences 2026, 16(4), 140; https://doi.org/10.3390/geosciences16040140 - 30 Mar 2026
Viewed by 447
Abstract
The Circum-Rhodope Belt fringes the Rhodope and Serbo-Macedonian zones in the Alpine orogen of the northern Aegean region. This belt contains Late Paleozoic and Mesozoic metasedimentary successions that record depositional history along the continental margin of Eurasia. Critical successions of the eastern Circum-Rhodope [...] Read more.
The Circum-Rhodope Belt fringes the Rhodope and Serbo-Macedonian zones in the Alpine orogen of the northern Aegean region. This belt contains Late Paleozoic and Mesozoic metasedimentary successions that record depositional history along the continental margin of Eurasia. Critical successions of the eastern Circum-Rhodope Belt, such as those exposed in the Fanari and Petrota areas, are studied here, integrating their structure, whole-rock geochemistry and U-Pb LA-ICP-MS zircon geochronological context. The Fanari turbiditic succession contains quartz arenite, while the Petrota succession consists of Fe-rich shale and sandstone, and both successions are distinguished by REE-depleted and REE-enriched characteristics and acidic and intermediate arc-related sedimentary sources, respectively. Detrital U-Pb zircon geochronology reveals a Late Carboniferous–Early Permian maximum depositional age of 301.2 ± 8.4 Ma for Fanari quartz arenite and a Late Jurassic maximum depositional age of 147.0 ± 2.0 Ma for Petrota Fe-shale. The results are interpreted in terms of Late Paleozoic continental slope deposition of the Fanari succession along the Eurasian margin and trench-arc sedimentation of the Petrota succession linked to the development of a Jurassic island arc system pertinent to the eastern Circum-Rhodope Belt. These tectonic settings and depositional environments can be used to restore an overall picture of a Late Paleozoic to Mid-Mesozoic sedimentation at the Rhodope–Serbo-Macedonian continental margin of Eurasia. Structures that developed in greenschist facies conditions and N-directed kinematics of the studied successions unequivocally relate them to other units of the eastern Circum-Rhodope Belt and its Late Jurassic tectonic evolution. Full article
Show Figures

Figure 1

Back to TopTop