RT Journal Article
T1 Indicadores estructurales y morfológicos de deformaciones postmiocenas en el sector occidental de la Falla de Crevillente (Cordillera Bética)
T1 Structural and morphological indicators of postmiocene deformations in the western Crevillente Fault (BeticCordillera)
A1 Canora Catalán, C.
A1 Martínez Díaz, J. J.
AB According to the NNW-SSE regional shortening direction active in the Eastern Betic Cordillera since theUpper Miocene, the ENE-WSW Crevillente Fault should be either blocked or locally reverse. However,dextral, sinestral or reverse movements have been reported along the fault zone. In this work, newobservations on the post-Miocene deformations of the Crevillente Fault are described. A block-tectonicsmodel active on different scales is proposed to explain the kinematics variability of the fault
PB Sociedad Geológica de España
YR 2005
FD 2005
LK http://hdl.handle.net/10272/8668
UL http://hdl.handle.net/10272/8668
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026