Rise, closure and reactivation of the Bicorb–Quesa evaporite diapir, eastern Prebetics, Spain

@inproceedings{Roca1996RiseCA,
  title={Rise, closure and reactivation of the Bicorb–Quesa evaporite diapir, eastern Prebetics, Spain},
  author={Eduard Roca and Pere Anad{\'o}n and R. Molina Utrilla and Antonio V{\'a}zquez},
  year={1996}
}
The Bicorb–Quesa diapir belongs to a complex system of evaporite diapirs located in the SE Iberian Peninsula. It was emplaced along the axis of a graben system flanked by two syn-diapir growth basins filled by Miocene sediments. The Miocene evolution of the diapir may be divided into three major phases: an initial extensional phase during which the graben system formed and the diapir rose; a second phase during which regional shortening closed the diapir; and a third phase characterized by… CONTINUE READING