Martín Pérez, J. A.Viseras, César2017-08-012017-08-011994http://hdl.handle.net/10272/14012The marly sediments traditionally known as "Cor Miocene" are located at the bottom of a very thick Middle Miocene detritic ensemble composed by clasts of alpujarride, malaguide and subbetic provenance. Locally they are overthrusted by Triassic Alpujarride dolostones. They are though to have been deposited In the foredeep basin related to the North-Betic Strait, located to the north of the Betic Internal ZonespaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Betic CordilleraNorth-Betic StraitCalcareous nannoplanktonMiddle Miocenejournal articleopen access