The Middle and Upper Oxfordian transgressive depositional sequence of Sierra de Cazorla, shows sorne sponge-calcareous stromatolite bioherms grown on a pelagic shelf (homoclinal ramp type). The geographical and temporal position is accurately defined and is mainly ra/ed by the deposition rate, the nature of the ground and the environmental energy.
© 2001-2026 Fundación Dialnet · Todos los derechos reservados