Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction

In continental margins, large-scale, strike-slip fault-systems resulted from oblique subduction commonly exhibit a complex pattern of faulting where major faults define the inland boundary of tectonic slivers that can be detached from the margin. In turn,

Detalles Bibliográficos
Autores: Veloso, E., Gomila, R., González, R., Cembrano, J., Jensen, E., Arancibia, G.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2015
País:Chile
Idioma:inglés
OAI Identifier:oai:repositorio.anid.cl:10533/238143
Acceso en línea:https://hdl.handle.net/10533/238143
Access Level:acceso abierto
Descripción
Sumario:In continental margins, large-scale, strike-slip fault-systems resulted from oblique subduction commonly exhibit a complex pattern of faulting where major faults define the inland boundary of tectonic slivers that can be detached from the margin. In turn,