Finite Element Stress Model of a Strike-Slip Duplex: A Case Study from Southern Chile.

dc.date.accessioned2019-03-27T15:56:51Z
dc.date.accessioned2022-10-18T22:07:10Z
dc.date.available2019-03-27T15:56:51Z
dc.date.available2022-10-18T22:07:10Z
dc.date.created2019-03-27T15:56:51Z
dc.date.issued2015
dc.identifierhttp://hdl.handle.net/10533/233627
dc.identifier1141139
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4464984
dc.description.abstractmargin, commonly driven by a transpressive regime of stress. They are often developed as a conjugate pair of master faults. Transverse structures, usually Riedel-like, connect both master faults, thus forming a structure known as strike-slip duplex. This
dc.languageeng
dc.relation14°
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1141139
dc.relationCongreso Geológico Chileno
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleFinite Element Stress Model of a Strike-Slip Duplex: A Case Study from Southern Chile.
dc.typePonencia


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