The bandurrias gabbro: late oligocene alkaline magmatism in the patagonian cordillera

dc.date.accessioned2017-03-23T17:39:49Z
dc.date.available2017-03-23T17:39:49Z
dc.date.created2017-03-23T17:39:49Z
dc.date.issued2005
dc.identifier0895-9811
dc.identifierhttp://hdl.handle.net/10533/176390
dc.identifier1000125
dc.identifierWOS:000227481100004
dc.languageeng
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD,
dc.relationhttps://doi.org/10.1016/j.james.2004.09.001
dc.relation10.1016/j.james.2004.09.001
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1000125
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.titleThe bandurrias gabbro: late oligocene alkaline magmatism in the patagonian cordillera
dc.typeArticulo


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