RT Journal Article
T1 Sobre la posición estratigráfica de las "Margas de Gor", Sierra de Baza, Cordillera Bética
T1 About the stratigraphic position of the "Gor Marls", Sierra de Baza, Betic Cordillera, Spain
A1 Martín Pérez, J. A.
A1 Viseras, César
AB 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
PB Sociedad Geológica de España
YR 1994
FD 1994
LK http://hdl.handle.net/10272/14012
UL http://hdl.handle.net/10272/14012
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026