Tectonic significance and hydrothermal fluid migration within a strike-slip duplex fault-vein network: an example from the Atacama Fault System

dc.creatorOlivares, Viviana
dc.creatorCembrano, José
dc.creatorArancibia Hernández, Gloria Cecilia
dc.creatorReyes Amaya, Nicolás Rafael
dc.creatorHerrera, Verónica
dc.creatorFaulkner, Daniel
dc.date.accessioned2020-11-29T23:46:37Z
dc.date.available2020-11-29T23:46:37Z
dc.date.created2020-11-29T23:46:37Z
dc.date.issued2010
dc.identifier10.5027/andgeoV37n2-a12
dc.identifier0718-7092
dc.identifierhttps://doi.org/10.5027/andgeoV37n2-a12
dc.identifierhttps://repositorio.uc.cl/handle/11534/49350
dc.languagees
dc.rightsacceso abierto
dc.subjectSistema de falla de Atacama
dc.subjectDeformación frágil
dc.subjectSistemas de vetas-fallas
dc.subjectDuplex Caleta Coloso
dc.subjectAtacama fault system
dc.subjectBrittle deformation
dc.subjectFault-veins systems
dc.subjectCaleta Coloso duplex
dc.titleTectonic significance and hydrothermal fluid migration within a strike-slip duplex fault-vein network: an example from the Atacama Fault System
dc.typeartículo


Este ítem pertenece a la siguiente institución