Three-dimensional resistivity image of the magmatic system beneath Lastarria volcano and evidence for magmatic intrusion in the back arc (northern Chile)

Geophysical Research Letters

dc.creatorDíaz, D.
dc.creatorHeise, W.
dc.creatorZamudio, F.
dc.date2020-03-11T20:26:55Z
dc.date2022-07-07T23:45:21Z
dc.date2020-03-11T20:26:55Z
dc.date2022-07-07T23:45:21Z
dc.date2015
dc.date.accessioned2023-08-21T21:44:36Z
dc.date.available2023-08-21T21:44:36Z
dc.identifier15090013
dc.identifier15090013
dc.identifierhttps://hdl.handle.net/10533/238146
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8286178
dc.descriptionLazufre volcanic center, located in the central Andes, is recently undergoing an episode of uplift, conforming one of the most extensive deforming volcanic systems worldwide, but its magmatic system and its connection with the observed uplift are still po
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.1002/2015GL064426
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.titleThree-dimensional resistivity image of the magmatic system beneath Lastarria volcano and evidence for magmatic intrusion in the back arc (northern Chile)
dc.titleGeophysical Research Letters
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


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