Evidencias de actividad diapírica sobre las unidades deposicionales del Maastrichtiense en la zona de Laño (Sur de Vitoria, cuenca Vasco-Cantábrica)

Abstract

The Laño quarry, situated near Vitoria in the south limb of the Miranda-Treviñ o Synclin orium , show san interesting section of Maastrichtian rocks which were re deposited in a variety of environments, such as marine, transitional and continental settings. These were directly influenced by the Pañacerrada diapir uplift as reflected by the numerous unconformities observed and their progressive relief towards the west