The central Red Sea is a nascent oceanic basin. Miocene evaporites, kilometers in thickness, were deposited during its continental rifting phase and early seafloor spreading. With further seafloor spreading, increasing dissolution due to increasing hydrothermal...
Carlos M. Duarte, Anders Røstad, Grégoire Michoud, Alan Barozzi, Giuseppe Merlino, Antonio Delgado‐Huertas, Brian C. Hession, Francis L. Mallon, Abdulakader M. Afifi, Daniele Daffonchio
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