Temporal evolution of the Darmadan salt diapir, eastern Fars region, Iran

A wide range of diapirs crop out along the eastern Fars region. They are constituted by the Pre-Cambrian to Early Cambrian Hormuz Fm. and located in the transition from the frontal structures of the Zagros fold-and-thrust belt and the Oman Ranges. While, in different previous works about the Persian...

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Veröffentlicht in:Tectonophysics 2019-09, Vol.766, p.115-130
Hauptverfasser: Snidero, Marco, Muñoz, Josep Anton, Carrera, Núria, Butillé, Mireia, Mencos, Joana, Motamedi, Hossein, Piryaei, Alireza, Sàbat, Francesc
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Sprache:eng
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