Journal Article10.1016/j.gloplacha.2024.104527
Contourite-like deposits suggest stronger-than-present circulation in the Plio-Pleistocene Red Sea
Neil C. Mitchell,Marco Ligi,Jonas Preine,Diederik Liebrand,Moamen Ali,Alessandro Decarlis +5 more
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About: This article is published in Global and Planetary Change. The article was published on 01 Jul 2024. The article focuses on the topics: Plio-Pleistocene & Contourite.
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Citations
Desiccation of the Red Sea basin at the start of the Messinian salinity crisis was followed by major erosion and reflooding from the Indian Ocean
Tihana Pensa,Antonio Delgado‐Huertas,Abdulkader M. Afifi +2 more
References
Red Sea isolation history suggested by Plio-Pleistocene seismic reflection sequences
TL;DR: In this article, a segment of Chirp sediment profiler data from the central Red Sea reveals prominent reflections at ∼1, ∼5, ∼23, ∼26 and ∼36 ms two-way travel time (TWT) from the seabed.
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On the Crossover of Boundary Currents in an Idealized Model of the Red Sea
TL;DR: In this paper, the authors investigated the mechanisms that produce and control the crossover in an idealized, eddy-resolving numerical model of the Red Sea and derived an analytical estimate for the crossover latitude.
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Tectono-Thermal Evolution of the Red Sea Rift
TL;DR: In this article, a regional interpolation protocol was employed to synthesize time-temperature reconstructions generated from the mined thermochronology data and burial histories produced from vitrinite reflectance and well data.
Geomorphological and geochemical evidence (230Th anomalies) for cross-equatorial currents in the central Pacific
Neil C. Mitchell,John M. Huthnance +1 more
- 01 Aug 2013
TL;DR: In this paper, shallow broad elongated sediment depressions and ridges are revealed in multibeam echo-sounder data collected over the carbonate ooze in the central equatorial Pacific.
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Expelled subsalt fluids form a pockmark field in the eastern Red Sea
Peter Feldens,Mark Schmidt,Isabell Mücke,Nico Augustin,Radwan Al-Farawati,Mohammad I. Orif,Eckhard Faber +6 more
TL;DR: In this paper, the authors aimed to constrain the source area of fluids responsible for the formation of a pockmark field in the eastern Red Sea, which extends over an area of at least 1,000 km2 at a water depth of ~400 m. The pockmarks have modal diameters of 140-150 m and are either randomly distributed on the seafloor or aligned within valleys approximately 25 m deep and several kilometres in length.
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