Editorial Board Members' Collection Series: “Sedimentology and Stratigraphy”

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

Deadline for manuscript submissions: 30 September 2025 | Viewed by 1447

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Department of Mathematical and Computer Sciences, Physical Sciences and Earth Sciences, University of Messina, 98166 Messina, Italy
Interests: forensic geology; geology; sedimentology; geological mapping; remote sensing; litho-biostratigraphy; structural geology; active tectonics; interplay of tectonics and sedimentation; carbonates; exploration geophysics; quaternary geology; geoheritage; geotourism
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Department of Science and Technology (DST), Università degli Studi del Sannio, 82100 Benevento, Italy
Interests: sedimentology; basin analysis; stratigraphy; field geology; wedge-top basins
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Special Issue Information

Dear Colleagues,

This Special Issue seeks to provide a comprehensive overview of the main advances in the field of sedimentology and stratigraphy. Sedimentology analyses the processes of formation, transport, deposition, and diagenesis of sediments and sedimentary rocks. Stratigraphy, based on the use  stratigraphic principles, explores how sediments and sedimentary rocks are accumulated in the diverse sedimentary environments widespread from marine environments to continental areas. Consequently, sedimentary rocks are recorders of the Earth’s ancient surface and its related evolution through space and time.

The main aims of the Special Issue will consist of bringing together research that studies sedimentological and stratigraphic data using advanced techniques, methods, and models with the goal of discussing wider contemporary implications. The Special Issue will cover topics concerning facies analysis, the processes of fluid transport, and petroleum geology, and links between erosion, deposition, climate, and tectonics.

Contributions from researchers worldwide that tackle key questions or comprehensive reviews of the current state of the art in sedimentology and stratigraphy are welcome.

We sincerely invite you to be part of this collaborative endeavor.

Dr. Roberta Somma
Dr. Sabatino Ciarcia
Guest Editors

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Keywords

  • sediment composition, texture, and structure
  • contamination of modern sediments
  • sedimentary structures
  • facies analysis
  • depositional systems
  • sequence stratigraphy
  • basin analysis
  • paleoenvironments
  • palaeoclimate
  • stratigraphic correlation
  • lithostratigraphy
  • biostratigraphy
  • geochronology
  • chronostratigraphy
  • magnetostratigraphy

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Published Papers (2 papers)

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Research

36 pages, 12719 KB  
Article
Petrogenesis and Provenance of the Triassic Metasedimentary Succession in the Sakar Unit, Bulgaria: Constraints from Petrology, Geochemistry, and U-Pb Detrital Geochronology
by Tzvetomila Filipova Vladinova and Milena Georgieva Georgieva
Geosciences 2025, 15(9), 343; https://doi.org/10.3390/geosciences15090343 (registering DOI) - 2 Sep 2025
Abstract
This study investigates the metasedimentary sequences of terrigenous–carbonate Sakar-type Triassic (TCSTT) and Sakar-type Triassic (STT) in the Sakar Unit, southeastern Bulgaria. Both share lithological similarities (alternation of carbonate–silicate schists, mica schists, marbles, and impure marbles) and are affected by post-Triassic metamorphism, but with [...] Read more.
This study investigates the metasedimentary sequences of terrigenous–carbonate Sakar-type Triassic (TCSTT) and Sakar-type Triassic (STT) in the Sakar Unit, southeastern Bulgaria. Both share lithological similarities (alternation of carbonate–silicate schists, mica schists, marbles, and impure marbles) and are affected by post-Triassic metamorphism, but with differences in metamorphic grade and partly in the variation of potential sources of the sedimentary material. STT shows a higher metamorphic grade (lower amphibolite facies) when compared to TCSTT (lower greenschist facies). Petrographic observations and geochemical analyses indicate protoliths composed of arkosic sandstones, shales, and limestones derived from a quartz-dominated source with minor contributions from intermediate magmatic sources. The U-Pb geochronology of the detrital zircons reveals a dominant Carboniferous age complemented by an Early Ordovician age, which is consistent with the presence of Carboniferous–Permian igneous rocks in the basement. The presence of Early Paleozoic and Cambrian–Neoproterozoic zircons in the detrital zircon populations suggests that older rocks of the basement of the Sakar Unit and the Srednogorie Zone are also sources of the sedimentary material. Based on the immobile trace element content and discrimination diagrams, the siliciclastic component originates from rocks formed in a continental-arc setting. REE patterns indicate a negative Eu anomaly inherited from granitic-source rocks. Full article
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38 pages, 13807 KB  
Article
A Sediment Provenance Study of Middle Jurassic to Cretaceous Strata in the Eastern Sverdrup Basin: Implications for the Exhumation of the Northeastern Canadian-Greenlandic Shield
by Michael A. Pointon, Helen Smyth, Jenny E. Omma, Andrew C. Morton, Simon Schneider, Stephen J. Rippington, Berta Lopez-Mir, Quentin G. Crowley, Dirk Frei and Michael J. Flowerdew
Geosciences 2025, 15(8), 313; https://doi.org/10.3390/geosciences15080313 - 12 Aug 2025
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Abstract
The Sverdrup Basin, Arctic Canada, is ideally situated to contain an archive of tectono-magmatic and climatic events that occurred within the wider Arctic region, including the exhumation of the adjacent (northeastern) part of the Canadian-Greenlandic Shield. To test this, a multi-analytical provenance study [...] Read more.
The Sverdrup Basin, Arctic Canada, is ideally situated to contain an archive of tectono-magmatic and climatic events that occurred within the wider Arctic region, including the exhumation of the adjacent (northeastern) part of the Canadian-Greenlandic Shield. To test this, a multi-analytical provenance study of Middle Jurassic to Cretaceous sandstones from the eastern Sverdrup Basin was undertaken. Most of the samples analysed were recycled from sedimentary rocks of the Franklinian Basin, with possible additional contributions from the Mesoproterozoic Bylot basins and metasedimentary shield rocks. The amount of high-grade metamorphic detritus in samples from central Ellesmere Island increased from Middle Jurassic times. This is interpreted to reflect exhumation of the area to the southeast/east of the Sverdrup Basin. Exhumation may have its origins in Middle Jurassic extension and uplift along the northwest Sverdrup Basin margin. Rift-flank uplift along the Canadian–West Greenland conjugate margin and lithospheric doming linked with the proximity of the Iceland hotspot and/or the emplacement of the Cretaceous High Arctic Large Igneous Province may have contributed to exhumation subsequently. The southeast-to-northwest thickening of Jurassic to Early Cretaceous strata across the Sverdrup Basin may be a distal effect of exhumation rather than rifting in the Sverdrup or Amerasia basins. Full article
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