Rising and falling diapirs, shifting depocenters, and flap overturning in the Cretaceous Sopeira and Sant Gervàs subbasins (Ribagorça Basin, southern Pyrenees)

The halokinetic structure of inverted salt‐related continental margins is frequently obliterated by compressional overprinting. The Cretaceous Sopeira and Sant Gervàs subbasins of the Ribagorça Basin (south central Pyrenees) show evidence of salt‐related extensional tectonics and diapiric growth alo...

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Veröffentlicht in:	Tectonics (Washington, D.C.) D.C.), 2016-03, Vol.35 (3), p.638-662
Hauptverfasser:	Saura, Eduard, Ardèvol i Oró, Lluís, Teixell, Antonio, Vergés, Jaume
Format:	Artikel
Sprache:	eng
Schlagworte:	Continental margins Cretaceous diapirism Diapirs flaps Jurassic Mesozoic minibasins Orogeny Plate tectonics Salts salt‐related margins Seismology southern Pyrenees
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