Detrital zircons from late paleozoic accretionary complexes in north-central chile (28 degrees-32 degrees s): possible fingerprints of the chilenia terrane

dc.date.accessioned2016-11-29T20:03:47Z
dc.date.available2016-11-29T20:03:47Z
dc.date.created2016-11-29T20:03:47Z
dc.date.issued2011
dc.identifier0895-9811
dc.identifierhttp://hdl.handle.net/10533/130499
dc.identifier1080468
dc.identifierWOS:000298464900016
dc.languageeng
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD,
dc.relationhttps://doi.org/10.1016/j.jsames.2011.06.002
dc.relation10.1016/j.jsames.2011.06.002
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1080468
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.titleDetrital zircons from late paleozoic accretionary complexes in north-central chile (28 degrees-32 degrees s): possible fingerprints of the chilenia terrane
dc.typeArticulo


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