Upper Pleistocene parabolic ridges (i.e. ‘chevrons’) from the Bahamas: Storm‐wave sediments or aeolian deposits? A quantitative approach
Author:
Affiliation:
1. Department of Earth Sciences University of Geneva Rue des Maraîchers 13 Geneva 1205 Switzerland
2. Department of Earth Sciences Carleton University 1125 Colonel by Drive Ottawa ON K1S 5B6 Canada
Funder
Université de Genève
Publisher
Wiley
Subject
Stratigraphy,Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12828
Reference134 articles.
1. Irregular fenestrae in Bahamian eolianites: a rainstorm‐induced origin;Bain R.;J. Sediment. Res.,1994
2. Lack of evidence for a substantial sea-level fluctuation within the Last Interglacial
3. GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments
4. “Chevrons” are not mega-tsunami deposits—A sedimentologic assessment
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1. Shallow carbonate geochemistry in the Bahamas since the last interglacial period;Earth and Planetary Science Letters;2024-02
2. Signatures of Pleistocene Marine Transgression Preserved in Lithified Coastal Dune Morphology of The Bahamas;Geosciences;2023-11-28
3. Parabolic dune distribution, morphology and activity during the last 20 000 years: A global overview;Earth Surface Processes and Landforms;2023-07-24
4. Coriolis effect recorded in Late Pleistocene Marine Isotope Stage 5e Bahamian aeolianites;Geology;2022-02-11
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