Slip distribution of the 2014 M-w=8.1 Pisagua, northern Chile, earthquake sequence estimated from coseismic fore-arc surface cracks

dc.date.accessioned2020-03-11T20:29:30Z
dc.date.accessioned2022-10-18T22:47:05Z
dc.date.available2020-03-11T20:29:30Z
dc.date.available2022-10-18T22:47:05Z
dc.date.created2020-03-11T20:29:30Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/238836
dc.identifier15110017
dc.identifierWOS:000386939800027
dc.identifierno scielo
dc.identifiers/i
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4470175
dc.description.abstractThe 2014 Mw = 8.1 Iquique (Pisagua), Chile, earthquake sequence ruptured a segment of the Nazca‐South America subduction zone that last hosted a great earthquake in 1877. The sequence opened >3700 surface cracks in the fore arc of decameter‐scale length a
dc.languageeng
dc.relationhttps://doi.org/10.1002/2016GL070284
dc.relation10.1002/2016GL070284
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.titleSlip distribution of the 2014 M-w=8.1 Pisagua, northern Chile, earthquake sequence estimated from coseismic fore-arc surface cracks
dc.typeArticulo


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