RT Journal Article
T1 Interpretación de la estructura de la zona NE de la cuenca de Madrid mediante datos gravimétricos
T2 Structure ofMadrid basin (NE zone) derived from gravity data
A1 Bergamín De La Viña, Juan Francisco
A1 Tejero López, Rosa
AB Modelling of five profiles in the NE area of Madrid Basin shows that low anomalies are related to both the thicker sediments infill of the Basin and the basement rocks like gneiss and grani tes. The highs are related to thick sequences of alternating slates and quarzites, outcropping or underlaying a thin caver. The main gradients are related to the marginal faults of the Basin. The existence of a granitic body and a NE-SW striking fault, was also detected. Out of the data obtained in the models, an isobaths map has been depicted of Madrid Basin which shows a fault bounded structure.
PB Seminario de Estudos Galegos. Area de Xeoloxía e Minería ;  Instituto Universitario de Xeoloxía "Isidro Parga Pondal"
SN 0213-4497
YR 1994
FD 1994
LK https://hdl.handle.net/20.500.14352/59884
UL https://hdl.handle.net/20.500.14352/59884
LA spa
NO España. Dirección General de Investigación Científica y Técnica
DS Docta Complutense
RD 10 abr 2025