Seismic hazard in low slip rate crustal faults, estimating the characteristic event and the most hazardous zone: study case San Ramón Fault, in southern Andes

Natural Hazards Earth Systems

dc.creatorEstay, N. P.
dc.creatorYáñez, G.
dc.creatorCarretier, S.
dc.creatorLira, E.
dc.creatorMaringue, J.
dc.date2020-03-11T20:27:02Z
dc.date2022-07-07T23:45:51Z
dc.date2020-03-11T20:27:02Z
dc.date2022-07-07T23:45:51Z
dc.date2016
dc.date.accessioned2023-08-22T05:39:30Z
dc.date.available2023-08-22T05:39:30Z
dc.identifier15090013
dc.identifier15090013
dc.identifierhttps://hdl.handle.net/10533/238188
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8324985
dc.descriptionCrustal faults located close to cities may induce catastrophic damages. When recurrence times are in the range of 1000-10000 or higher, actions to mitigate the effects of the associated earthquake are hampered by the lack of a full seismic record, and in
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.5194/nhess-16-2511-2016
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleSeismic hazard in low slip rate crustal faults, estimating the characteristic event and the most hazardous zone: study case San Ramón Fault, in southern Andes
dc.titleNatural Hazards Earth Systems
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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