Quaternary marine and continental sedimentation in the northern Red Sea and Gulf of Suez (Egyptian coast): influences of rift tectonics, climatic changes and sea-level fluctuations

Plaziat, J.-C.; Baltzer, F.; Choukri, A.; Conchon, O.; Freytet, P.; Orszag-Sperber, F.; Raguideau, A.; Reyss, J.-L.

doi:10.1007/978-94-011-4930-3_29

Cited by 73Marine and environmental studiesGeology and Paleoclimatology ResearchGeological formations and processes

Quaternary marine and continental sedimentation in the northern Red Sea and Gulf of Suez (Egyptian coast): influences of rift tectonics, climatic changes and sea-level fluctuations

Plaziat, J.-C., Baltzer, F., Choukri, A., Conchon, O., Freytet, P., Orszag-Sperber, F., Raguideau, A., Reyss, J.-L.·1998·Sedimentation and Tectonics in Rift Basins Red Sea:- Gulf of Aden

DOI 10.1007/978-94-011-4930-3_29

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The region of the Farasan Islands and Jizan on the adjacent mainland is located above an uplifting salt dome, while the offshore topography of the Farasan Islands has a number of deep depressions resulting from salt solution.
“The region of the Farasan Islands and Jizan on the adjacent mainland is located above an uplifting salt dome, while the offshore topography of the Farasan Islands has a number of deep depressions resulting from salt solution (Bosence et al. 1998; Plaziat et al. 1998; Warren 1999).”
From Coastlines, Submerged Landscapes, and Human Evolution: The Red Sea Basin and the Farasan Islands (2007) · cites this paper as Plaziat et al. 1998
Evidence from many locations of elevated marine beach deposits dated to the Last Interglacial at heights above present sea level of c. 5 m, close to the global norm, strengthens the inference that for much of the Red Sea there has been little overall vertical movement of the rift flanks during the past 125,000 years.
“This is consistent with the evidence from many locations of elevated marine beach deposits dated to the Last Interglacial at heights above the present sea level of c. 5 m (e.g. Gvirtzman 1994; Plaziat et al. 1998) close to the global norm, which strengthens the inference that for much of the Red Sea there has been little overall vertical movement of the rift flanks during the past 125,000 years.”
From Coastlines, Submerged Landscapes, and Human Evolution: The Red Sea Basin and the Farasan Islands (2007) · cites this paper as Plaziat et al. 1998

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Authors: Plaziat, J.-C., Baltzer, F., Choukri, A., Conchon, O., Freytet, P., Orszag-Sperber, F., Raguideau, A., & Reyss, J.-L.
Affiliations: Royal Holloway University of London (GB)
Université Paris-Sud (FR)
Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR)
ORCID: Choukri, A.
Venue: Sedimentation and Tectonics in Rift Basins Red Sea:- Gulf of Aden
Publisher: Springer Netherlands
Published: 1998
Pages: 537-573
DOI: 10.1007/978-94-011-4930-3_29
OpenAlex: W45179253
Cited by: 73
References: 0
Citations by year: 2025: 4 · 2024: 6 · 2023: 11 · 2022: 5 · 2021: 2 · 2020: 4 · 2019: 3 · 2018: 3 · 2017: 3 · 2016: 3 · 2015: 2 · 2014: 1 · 2013: 2 · 2012: 2
FWCI: 1.90
Type: book chapter
Language: en
Open access: closed
Locations: Springer eBooks (publishedVersion)
HAL (submittedVersion)
Topics: Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and environmental studies
Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
Keywords: Quaternary sedimentation, marine sediment, continental deposits, rift tectonics, sea-level fluctuations, glacio-eustasy, paleoclimate, U-Th dating, coral reefs, sea urchins, gypsum, Early Pleistocene, Holocene, Gulf of Suez, Red Sea, rifting

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Quaternary marine and continental sedimentation in the northern Red Sea and Gulf of Suez (Egyptian coast): influences of rift tectonics, climatic changes and sea-level fluctuations

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