RT Journal Article
T1 Tectónica extensional en el Sistema Central: la Zona de Cizalla Dúctil de Santa María de la Alameda (Madrid)
A1 Capote Del Villar, Ramón
A1 Martín González, Fidel
A1 Tsige Beyene, Meaza
AB The Santa Maria de Alameda (Madrid) Ductile Shear Zone is a complex mylonitic belt trending east -West and dipping 30°-60° southward. The hanging wall block sinks towards the South-Southeast. Its kinematics is in relation to an extensional tectonic regime with North-south stretching direction. This large structure belongs to the early stages of the Malagon tectonic period, where important faulting and dike emplacement were produced. The shearing process was developed in retrograde metamorphic conditions in a wide range of temperature, which goes from 400° C to 150° C. The age of this deformation is constrained by the variscan regional metamorphic peak and the intrusion of late variscan granitoids (Las Navas del Marques adamellites), being therefore, between early Namurian and Stephanian.
PB Sociedad Geológica de España
SN 0213-683X
YR 2000
FD 2000
LK https://hdl.handle.net/20.500.14352/107291
UL https://hdl.handle.net/20.500.14352/107291
LA spa
NO Capote del Villar, R., Martín González, F. y Tsige Beyene, M. (2000): «Tectónica extensional en el Sistema Central: La Zona de Cizalla Dúctil de Santa María de la Alameda (Madrid)», Geogaceta, 28, pp. 27-30.
DS Docta Complutense
RD 14 dic 2025