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 524

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Guest Editor
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

Manuscript Submission Information

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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 (1 paper)

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Research

38 pages, 13807 KiB  
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 (registering DOI) - 12 Aug 2025
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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