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

dc.date.accessioned2020-03-11T20:26:55Z
dc.date.accessioned2022-10-18T22:41:53Z
dc.date.available2020-03-11T20:26:55Z
dc.date.available2022-10-18T22:41:53Z
dc.date.created2020-03-11T20:26:55Z
dc.date.issued2015
dc.identifierhttp://hdl.handle.net/10533/238146
dc.identifier15090013
dc.identifierWOS:000358691300017
dc.identifierno scielo
dc.identifiereid=2-s2.0-84938216209
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469485
dc.description.abstractLazufre 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.languageeng
dc.relationhttps://doi.org/10.1002/2015GL064426
dc.relation10.1002/2015GL064426
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.titleThree-dimensional resistivity image of the magmatic system beneath Lastarria volcano and evidence for magmatic intrusion in the back arc (northern Chile)
dc.typeArticulo


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