Un ejemplo de tectónica salina: el sector NE del Surco de Valencia

Abstract

The messinian salt develops salt rollers, pillows and diapirs in the linking zone between the Valencia Trough and the Provenga! Basin. The correlation of the different structures based on the sedimentary wedges linked to the salt rollers formation, the onlap surfaces and truncations, as well as a sequential restitution of the salt structures allows us to propose different origins for the salt structures of different areas of the basin