Sobre la posición estratigráfica de las "Margas de Gor", Sierra de Baza, Cordillera Bética
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Abstract
The 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 Zone
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