2022
DOI: 10.1016/j.sedgeo.2022.106121
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Syn-rift sedimentary response to growth folding along a rift-margin transfer zone: An example from the early Miocene of the Gulf of Suez, Egypt

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Cited by 6 publications
(6 citation statements)
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“…2%; Table 2, %VF), consistent with that concluded by Barrett et al. (2021) for the Thebe‐2 fault system (i.e., 10%), and from field‐based in the Gulf of Suez, Egypt (i.e., 1%–8%; Badr et al., 2022; Strachan et al., 2013). Additional depositional processes may have supplied sediment, such as the introduction of extra‐basinal material by bottom currents and/or suspension settling of pelagic and hemipelagic material (e.g., units 1b, 2d, 3, and 4b; Table 3; Appendix 4, Table 5), and source areas like hangingwall‐derived sediment (e.g., Unit 2b; Table 3, Appendix 4, Table 5) or relay‐ramps related to fault overlap supply the remaining syn‐rift hangingwall fill (ca.…”
Section: Discussionsupporting
confidence: 87%
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“…2%; Table 2, %VF), consistent with that concluded by Barrett et al. (2021) for the Thebe‐2 fault system (i.e., 10%), and from field‐based in the Gulf of Suez, Egypt (i.e., 1%–8%; Badr et al., 2022; Strachan et al., 2013). Additional depositional processes may have supplied sediment, such as the introduction of extra‐basinal material by bottom currents and/or suspension settling of pelagic and hemipelagic material (e.g., units 1b, 2d, 3, and 4b; Table 3; Appendix 4, Table 5), and source areas like hangingwall‐derived sediment (e.g., Unit 2b; Table 3, Appendix 4, Table 5) or relay‐ramps related to fault overlap supply the remaining syn‐rift hangingwall fill (ca.…”
Section: Discussionsupporting
confidence: 87%
“… Note : Facies analysis and characteristics of the interpreted seismic units. Base‐of‐scarp deposits analogues: early Miocene of the Gulf of Suez, Egypt (Badr et al., 2022); hangingwal‐derived prograding deposits analogues: El Qaa fault block, Suez Rift, Egypt (Muravchik et al., 2018). …”
Section: Resultsmentioning
confidence: 99%
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