Fault Zone Dynamic Processes: Evolution of Fault Properties During Seismic Rupture

dc.date.accessioned2020-03-11T20:27:05Z
dc.date.accessioned2022-10-18T22:42:18Z
dc.date.available2020-03-11T20:27:05Z
dc.date.available2022-10-18T22:42:18Z
dc.date.created2020-03-11T20:27:05Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/238201
dc.identifier15090013
dc.identifierWOS:000441290800004
dc.identifierno scielo
dc.identifiers/i
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469540
dc.description.abstractSeismogenic fault fracturing can create considerable fracture permeability in and around fault zones initiating large fluxes of fluid, particularly at fault terminations and dilatational jogs. In this work we show that fluids can also be channeled and pot
dc.languageeng
dc.relationhttps://doi.org/10.1002/9781119156895
dc.relation10.1002/9781119156895
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.titleFault Zone Dynamic Processes: Evolution of Fault Properties During Seismic Rupture
dc.typeArticulo


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