Salt-related deformations in the Deep Antalya Basin: Preliminary results of the Mac Gan Cruise
作者： Marco Taviani , Sergio Rossi
DOI: 10.1016/0025-3227(89)90141-2
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摘要: Abstract Seismic investigation of the Deep Antalya Basin shows contribution halokinesis Messinian salt in shaping shallow morphological setting area. The causes such salt-related deformations are difficult to firmly establish. Plio-Quaternary overburden (∼200–250 ms) seems too little be responsible for extensive diapirism so widespread Basin; extensional tectonics may therefore involved some degree. There indications that bears two separate layers. In this case, a significant form sum sediments and younger evaporites present, with older layer most observed doming.
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