Geophysical Research Letters

dc.creatorDe Pascale, G. P.
dc.creatorChandler-Yates, N.
dc.creatorDela Pena, F.
dc.creatorWilson, P.
dc.creatorMay, E.
dc.creatorTwiss, A.
dc.creatorCheng, C.
dc.date2020-03-11T20:27:01Z
dc.date2022-07-07T23:45:49Z
dc.date2020-03-11T20:27:01Z
dc.date2022-07-07T23:45:49Z
dc.date2016
dc.date.accessioned2023-08-23T00:16:17Z
dc.date.available2023-08-23T00:16:17Z
dc.identifier15090013
dc.identifier15090013
dc.identifierhttps://hdl.handle.net/10533/238185
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8354475
dc.descriptionThe 300 km long South Westland Fault Zone (SWFZ) is within the footwall of the Central Alpine Fault (<20 km away) and has 3500m of dip-slip displacement, but it has been unknown if the fault is active. Here the first evidence for SWFZ thrust faulting in t
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.1002/2016GL068233
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.titleActive tectonics west of New Zealand ́s Alpine Fault: South Westland Fault Zone activity shows Australian Plate instability.
dc.titleGeophysical Research Letters
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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