Submarine earthquake rupture, active faulting and volcanism along the major Liquiñe-Ofqui Fault Zone and implications for seismic hazard assessment in the Patagonian Andes.

dc.date.accessioned2020-03-11T20:26:39Z
dc.date.accessioned2022-10-18T22:41:25Z
dc.date.available2020-03-11T20:26:39Z
dc.date.available2022-10-18T22:41:25Z
dc.date.created2020-03-11T20:26:39Z
dc.date.issued2013
dc.identifierhttp://hdl.handle.net/10533/238085
dc.identifier15090013
dc.identifierWOS:000319975200007
dc.identifierS0718-71062013000100007
dc.identifiereid=2-s2.0-84874729727
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469424
dc.description.abstractThe Liquiñe-Ofqui fault zone (LOFZ) in the Patagonian Andes is an active major transpressional intra-arc fault system along which Quaternary faulting and volcanism develop. Subaerial and submarine geomorphologic and structural characterization of latest P
dc.languageeng
dc.relation10.5027/andgeoV40n1-a07
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.titleSubmarine earthquake rupture, active faulting and volcanism along the major Liquiñe-Ofqui Fault Zone and implications for seismic hazard assessment in the Patagonian Andes.
dc.typeArticulo


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