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- W88693731 abstract "The Triassic Paleotethys was a wedge-like ocean opening to the east, which was totally eliminated during the early Mesozoic by subduction along the Cimmerian and Indosinian suture zone. The Tethys, s.s., was an Early Jurassic creation formed when Africa moved east relative to Europe. The sinistral movement of Africa continued until Late Cretaceous when the movement became dextral. The closing of the gap between Africa and Europe led to the Alpine orogeny and the elimination of much of the Tethys. Only the eastern Mediterranean Ionian and Levantine basins are left as possible relics of this Mesozoic ocean. The western Mediterranean and the Aegean are post-orogenic basins. The Balearic Basin was created during late Oligocene or earliest Miocene time by rifting tectonics. The Tyrrhenian Basin was probably somewhat younger. The presence of oceanic tholeiites under its abyssal plain indicates that submarine basalt volcanism played a major role in the genesis of this basin. The Aegean Basin is probably the youngest and has undergone considerable Pliocene-Quaternary subsidence. Tectonic synthesis indicates that the Mediterranean basins, except perhaps the Aegean, were in existence and deep prior to the Messinian Salinity Crisis." @default.
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- W88693731 date "1978-01-01" @default.
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- W88693731 title "GENESIS OF THE TETHYS AND THE MEDITERRANEAN" @default.
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