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Isotopic indicators of deformation in the Red Sea
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“This approach has yielded evidence of a major tectonic event prior to 40,000 years ago but none subsequently, and suggests that tectonic widening of the Red Sea has been more modest for the last 40,000 years and possibly longer .”
From Coastlines, Submerged Landscapes, and Human Evolution: The Red Sea Basin and the Farasan Islands (2007) · cites this paper as Vita-Finzi and Spiro 2006
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References 55 · Cited by 4
Research works printed but not linked: 45
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Metadata
- Authors
- Vita-Finzi, C., & Spiro, B.
- Affiliations
- Natural History Museum (GB)
- ORCID
- Spiro, Baruch
- Venue
- Journal of Structural Geology
- Publisher
- Elsevier BV
- Published
- 2006-06
- Volume
- 28
- Issue
- 6
- Pages
- 1114-1122
- ISSN
- 0191-8141 (ISSN-L)
- OpenAlex
- W2145718937
- Cited by
- 4
- References
- 55
- Citations by year
- 2023: 1
- FWCI
- 1.19
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Structural Geology (publishedVersion)
- Funders
- Woods Hole Oceanographic Institution
- Ocean Life Institute, Woods Hole Oceanographic Institution
- University College London
- Natural Environment Research Council
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- paleostress analysis, Red Sea, extensional deformation, rifting
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