Magmatism as a probe to the neogene shallowing of the nazca plate beneath the modern chilean flat-slab

dc.date.accessioned2017-03-23T15:14:48Z
dc.date.available2017-03-23T15:14:48Z
dc.date.created2017-03-23T15:14:48Z
dc.date.issued2002
dc.identifier0895-9811
dc.identifierhttp://hdl.handle.net/10533/173279
dc.identifier1990009
dc.identifierWOS:000175725400005
dc.languageeng
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD,
dc.relationhttps://doi.org/10.1016/S0895-9811(02)00005-6
dc.relation10.1016/S0895-9811(02)00005-6
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1990009
dc.relationinfo:eu-repo/semantics/dataset/hdl.handle.net/10533/93477
dc.relationinstname: Conicyt
dc.relationreponame: Repositorio Digital RI2.0
dc.relationinstname: Conicyt
dc.relationreponame: Repositorio Digital RI2.0
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleMagmatism as a probe to the neogene shallowing of the nazca plate beneath the modern chilean flat-slab
dc.typeArticulo


Este ítem pertenece a la siguiente institución