RT Journal Article
T1 Partición de la deformación cenozoica intraplaca en el Sistema Central
T1 Cenozoic intraplate strain partitioning in the Central System
A1 Vicente, Gerardo de
AB A new model for Cenozoic strain partitioning is proposed here for the Central System at the Messejana(Plasencia) fault zone. It explains the simultaneous movement of parallel NE-SW trending thrust and strikeslipfaults within a global N-S compression. This process could account for local bends in the shmax trajectories,from NW-SE trending close to the Ponsul-Gata and Gredos thrusts to NE-SW trending along the Messejanaleft-lateral strike-slip fault. This structural pattern may change current thinking with regard to the paleostressevolution of the Iberia foreland during the Cenozoic
YR 2009
FD 2009
LK http://hdl.handle.net/10272/8108
UL http://hdl.handle.net/10272/8108
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026