Tectonic Evolution and Paleogeography of Plate Boundaries

A special issue of Geosciences (ISSN 2076-3263).

Deadline for manuscript submissions: closed (30 September 2024) | Viewed by 1843

Special Issue Editors


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Guest Editor
Department of Geography and Geology, University Salzburg, 5020 Salzburg, Austria
Interests: plate tectonic reconstruction; mountain building; geochronology; structural processes; provenance studies; sedimentary basins; petrochronology

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Guest Editor
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Submarine Geoscience and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
Interests: tectonics; orogenic belt; structure analysis; coupling of basin and mountain; continental marginal tectonic process

Special Issue Information

Dear Colleagues,

We are pleased to announce the launch of a Special Issue titled "Tectonic Evolution and Paleogeography of Plate Boundaries". This Special Issue presents a collection of cutting-edge research and advancements in understanding the Earth's past geographies and the processes that have shaped its tectonic evolution. The main emphasis is on plate boundary processes, which juxtapose tectonic units of different paleogeographic origin through superimposed tectonic processes.

The articles in this Special Issue cover a wide range of topics, including paleogeographic reconstructions, plate tectonics, paleoclimatology, sedimentary basin analysis, petrochronology, and provenance studies and aim to serve as a comprehensive resource for researchers, geoscientists, and anyone interested in Earth's geological past.

Contributions to this Special Issue will be rigorously peer-reviewed to ensure the highest quality of research and scholarship. We invite researchers to submit their latest findings and insights surrounding the complex interplay between geology, climate, and tectonic processes that have influenced the development of our planet.

We look forward to receiving your submissions and publishing the latest advancements in paleogeography and tectonic evolution.

Prof. Dr. Franz Neubauer
Prof. Dr. Yongjiang Liu
Guest Editors

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Keywords

  • paleogeography
  • tectonic evolution
  • structural geology
  • paleoclimatology
  • sedimentary petrology
  • petrochronology
  • geochronology

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Published Papers (1 paper)

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Research

16 pages, 14559 KiB  
Article
Heavy Minerals Distribution and Provenance in Modern Beach and Fluvial Sands of the Betic Cordillera, Southern Spain
by Anna Chiara Tangari, Daniele Cirillo, Raffaella De Luca, Domenico Miriello, Elena Pugliese and Emilia Le Pera
Geosciences 2024, 14(8), 208; https://doi.org/10.3390/geosciences14080208 - 5 Aug 2024
Cited by 1 | Viewed by 1392
Abstract
This study uses heavy detrital minerals to determine actualistic fluvial and beach sand provenance across the Betic Cordillera (Spain), along the coast from Almeria to Marbella. The Betic Cordillera, primarily composed of metamorphic rocks to the east, supply an assemblage dominated by almandine [...] Read more.
This study uses heavy detrital minerals to determine actualistic fluvial and beach sand provenance across the Betic Cordillera (Spain), along the coast from Almeria to Marbella. The Betic Cordillera, primarily composed of metamorphic rocks to the east, supply an assemblage dominated by almandine and graphite, with a longshore dispersal from Almeria to Malaga. Buergerite and hypersthene indicate the provenance of calcalkaline lavas east of Cabo de Gata. The western part of the Betic Cordillera, which comprises the Ronda Peridotite Complex, supplies a chromite and diopside assemblage, with a dispersal from Marbella to Algeciras. Considering these mineralogical suites, the effects of source rock compositions and weathering are evaluated. The heavy mineral species mirror the mineralogy of the source rocks of local outcrops and wider source terranes. The fluvial heavy mineral suites do not differ significantly from those in the beaches except for some unstable species. Unstable species such as olivine, pyroxene, and amphibole do not show evidence of loss because of elevated topography and semiarid climate, which do not affect heavy minerals. This contribution also evaluates the potential of some heavy detrital species as ideal pathfinders in searching for diamonds. Full article
(This article belongs to the Special Issue Tectonic Evolution and Paleogeography of Plate Boundaries)
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