A new work to illustrate a strike-slip basin in the Betics. Here the link to the publisher. The Agost Basin is characterized by a Miocene-Quaternary shallow marine and continental infilling controlled by the evolution of several curvilinear faults involving salt tectonics derived from Triassic rocks. From the Serravallian on, the area experienced a horizontal maximum compression […]

Continuar leyendo sobre The Agost Basin (Betic Cordillera, Alicante province, Spain): a pull-apart basin involving salt tectonics