The Tectonic Origins of Sedimentary Basins: Provenance and Evolution Across Geological Time

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

Deadline for manuscript submissions: 30 April 2025 | Viewed by 1131

Special Issue Editors


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1. Civil Engineering Department (DINCi), University of Calabria, 87036 Arcavacata di Rende, Italy
2. Laboratory of Remote Sensing and Planetology, University of Chieti-Pescara, 66100 Chieti, Italy
Interests: sedimentary geology; provenance; sedimentary petrography heavy minerals; mineralogy and geochemistry of soils and sediments; weathering; planetary sciences

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Guest Editor
1. Laboratory of Structural Geology, 3D Digital Cartography and Geomatics, University of Chieti-Pescara, 66100 Chieti, Italy
2. CRUST Centro InteR, Universitario per L’analisi Sismotettonica Tridimensionale, 66100 Chieti, Italy
Interests: 3D geological model building; seismotectonics; seismic hazard; earthquake geology; active tectonics, structural geology, remote sensing; UAV photogrammetry in RTK/PPK; GNSS data analyses; field digital-geological mapping; GIS-data processing, Sedimentary Geology
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Guest Editor
Associate Professor, Department of Biology, Ecology and Earth Sciences (DiBEST), University of Calabria, 87036 Arcavacata di Rende, Italy
Interests: siliciclastic sediments and sedimentary rocks; sand(stone) composition and provenance; petrography and origin of sand(stone) types
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Associate Professor, Laboratory of Remote Sensing and Planetology, University of Chieti-Pescara, 66100 Chieti, Italy
Interests: planetary sciences; planetary explorations; remote sensing; sedimentary environment

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Guest Editor
1. Associate Professor, Laboratory of Structural Geology, 3D Digital Cartography and Geomatics, University of Chieti-Pescara, 66100 Chieti, Italy
2. CRUST Centro InteRUniversitario per L’analisi Sismotettonica Tridimensionale, 66100 Chieti, Italy
Interests: earthquake rupture process; tectonic geomorphology; structural geological analysis
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

The interaction between tectonics and sedimentary basin evolution is a fundamental process that shapes the Earth's surface. Sedimentary basins serve as archives of geological history, recording the dynamic processes that govern the Earth's crust over time. Understanding the tectonic origins and evolution of these basins and the provenance of the sediments that fill them is crucial for reconstructing past and recent environments, tectonic regimes, and paleogeography.

On a global scale, advancements in sand(stone) petrography have provided critical insights for interpreting tectonic setting models, unraveling (paleo)climatic conditions of source areas, whilst understanding and analyzing facies relationships within stratigraphic units. Moreover, these studies contribute to quantifying the overall volume of clastic units within basin fills.

This Special Issue invites multidisciplinary research investigating the complex relationships between tectonics, sedimentary basin formation, and sediment provenance. We encourage contributions that explore these processes across various geological settings and time periods, shedding light on how tectonic forces influence basin evolution and how sedimentary records reveal the history of the Earth's crust. Contributions are also welcome on sedimentary processes on other planetary surfaces, which can be considered terrestrial analogues.

This Special Issue will focus on the following key themes:

  • Tectonic controls on basin formation;
  • Sedimentary provenance and tectonic evolution through geological time;
  • Geodynamic modeling of basin formation;
  • Implications for natural resources and geohazards.

Dr. Anna Chiara Tangari
Prof. Dr. Daniele Cirillo
Assoc. Prof. Dr. Emilia Le Pera
Assoc. Prof. Dr. Lucia Marinangeli
Assoc. Prof. Dr. Francesco Brozzetti
Guest Editors

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Keywords

  • sedimentary basins
  • provenance
  • sediment erosion and transport
  • paleogeography and paleoclimatology
  • stratigraphy and tectono-stratigraphy
  • sedimentary petrography
  • mineralogy and geochemistry of sedimentary rocks
  • three-dimensional geological modeling
  • tectonics
  • geo-hazards

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Published Papers (1 paper)

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Research

16 pages, 42046 KiB  
Article
Characterisation of Fault-Related Mn-Fe Striae on the Timpa Della Manca Fault (Mercure Basin, Southern Apennines, Italy)
by Sabrina Nazzareni, Luciana Mantovani, Mattia Pizzati, Danilo Bersani, Tiziano Boschetti, Ambra Palmucci, Daniele Cirillo and Francesco Brozzetti
Geosciences 2024, 14(11), 299; https://doi.org/10.3390/geosciences14110299 - 5 Nov 2024
Viewed by 698
Abstract
The Quaternary Mercure basin is a complex fault structure located in the Pollino region of the southern Apennines (Italy). A persistent seismic gap makes the Mercure basin structure one of Italy’s highest seismic risk zones. The southernmost termination of the Mercure basin is [...] Read more.
The Quaternary Mercure basin is a complex fault structure located in the Pollino region of the southern Apennines (Italy). A persistent seismic gap makes the Mercure basin structure one of Italy’s highest seismic risk zones. The southernmost termination of the Mercure basin is the Timpa della Manca fault. The fault’s mirror is characterised by distinctive, lineated, black-coloured striae decorating a cataclasite made of carbonate clasts. These black-coloured striae consist of a mixture of Mn phases, including hollandite, todorokite, birnessite, and orientite, which are associated with goethite and hematite along with minor amounts of phyllosilicates (chlorite, muscovite), quartz, and sursassite. This mineral association and their phase stability suggest that hydrothermal circulating fluids may have mobilised and re-precipitated low-temperature Mn hydrous phases within the shear zone, leaving remnants of higher-temperature minerals. Oceanic crust remnant blocks within the Frido Unit appear to be the most likely source of the Mn. The uniqueness of the Mn striae on the Timpa della Manca fault offers intriguing insights into fluid circulation within the Mercure basin tectonic system, with potential implications for the seismotectonic characteristics of the Pollino region. Full article
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