RT Journal Article
T1 La tectónica alpina en el sector centro-oriental del borde norte del Sistema Central (provincia de Segovia, España)
T1 The alpine tectonics in the middle eastern area of the northern edge of the Central System (Segovia province, Spain)
A1 Gómez Ortiz, David
A1 Babín, Rosa
AB A microstructural analysis has been completed in the Northern edge of the Spanish Central System (Segovia province). The analysis is based op the study of 5 sites of homogeneously-distributed faults, which are located either in Paleozoic or Mesozoic rocks, or in both of them. Altogether, 7 62 couples of fault-striae have been measured- The fault population analysis methods that have been applied on them are the following: slip model (Reches, 1983; De Vicente, 7 988); right dieder method (Angelier y Mechler, 1977) and Delvaux (1993). The comparison of the results obtained from the different methods has made possible to find out the shortening direction and the shape and orientation of the stress tensor for each Station. Two different tensors have been defined. A extensional ope, having a compression direction EO, attributed to the Hiendelaepcina phase, and a transpressive one with a compression direction N 160 E, corresponding to the Guadarrama phase
PB Sociedad Geológica de España
YR 1995
FD 1995
LK http://hdl.handle.net/10272/13417
UL http://hdl.handle.net/10272/13417
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026