Geophysical Research Letters

dc.creatorLoveless, J. P.
dc.creatorScott, C. P.
dc.creatorAllmendinger, R. W.
dc.creatorGonzalez, G.
dc.date2020-03-11T20:29:30Z
dc.date2022-07-07T23:54:50Z
dc.date2020-03-11T20:29:30Z
dc.date2022-07-07T23:54:50Z
dc.date2016
dc.date.accessioned2023-08-22T00:17:29Z
dc.date.available2023-08-22T00:17:29Z
dc.identifier15110017
dc.identifier15110017
dc.identifierhttps://hdl.handle.net/10533/238836
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8299873
dc.descriptionThe 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.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.1002/2016GL070284
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.titleSlip distribution of the 2014 M-w=8.1 Pisagua, northern Chile, earthquake sequence estimated from coseismic fore-arc surface cracks
dc.titleGeophysical Research Letters
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


Este ítem pertenece a la siguiente institución