Articulo
Exploring the shallow structure of the San Ramón thrust fault in Santiago, Chile (∼33.5° S), using active seismic and electric methods
Fecha
2014Registro en:
15090013
WOS:000347545800019
no scielo
eid=2-s2.0-84940316543
Institución
Resumen
The crustal-scale west-vergent San Ramón thrust fault system at the foot of the main Andean Cordillera in central Chile is a geologically active structure with Quaternary manifestations of complex surface rupture along fault segments in the eastern bor- d