RT Journal Article
T1 Anomalías gravimétricas y magnéticas en la Depresión de Granada (Cordilleras Béticas): tratamiento e interpretación
T1 Gravity and magnetic anomalies in the Granada Depression (Betic Cordilleras): Processing and interpretation
A1 Jiménez Pintor, J.
A1 Galindo Zaldívar, Jesús
A1 Ruano, Patricia
A1 Morales, J.
AB The Granada Depression, located in the central sector of the Betic Cordilleras, is an intramountain depression filled mainly by detritic, evaporite and carbonate rocks since Miocene. Gravity anomaly minima are associated to the main depocentres or to the Triassic rocks of Keuper facies, located in the basin basement. Gravity models show the asymmetric character of most of the depocenters, that constitute half-graben structures bounded by normal faults. These faults are responsible of the structure of the basin and have developed mainly in a NE-SW extensional setting. The most intense magnetic anomalies are located in the southeastern sector of the Depression and are related to shallow bodies of amphibole schists of the Alpujarride Complex
PB Sociedad Geológica de España
YR 2001
FD 2001
LK http://hdl.handle.net/10272/9405
UL http://hdl.handle.net/10272/9405
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 29 may 2026