dc.contributorRabassa, Jorge Oscar
dc.creatorAcevedo, Rogelio Daniel
dc.date.accessioned2020-12-01T19:48:18Z
dc.date.accessioned2022-10-15T07:50:47Z
dc.date.available2020-12-01T19:48:18Z
dc.date.available2022-10-15T07:50:47Z
dc.date.created2020-12-01T19:48:18Z
dc.date.issued2019
dc.identifierAcevedo, Rogelio Daniel; The Magmatic Rocks Probably Corresponding to the Andean Batholith and the Associated Metamorphic Contact Phenomena; Springer; 2019; 83-93
dc.identifier978-3-030-00165-0
dc.identifierhttp://hdl.handle.net/11336/119491
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4362414
dc.description.abstractThe knowledge about the presence of outcropping plutonic rocks in the Argentine side of the Fuegian Andes is limited exclusively to the references about the dioritic bodies, in a wider sense, of Mount Jeu Jepén (immediately to the ESE of Lake Fagnano), Spion Kop (in the Lucas Bridges Range, on Paso Harberton) hills and Estancia Túnel, to the E of Ushuaia (this intrusive was attributed to the Andean Batholith and it would be comparable or not with those of the Santa Rosa Plutonic Complex).
dc.languageeng
dc.publisherSpringer
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007%2F978-3-030-00166-7_9
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1007/978-3-030-00166-7_9
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.sourceGeological Records of the Fuegian Andes Deformed Complex Outlined in a Patagonian Orogenic Belt Regional Context
dc.subjectPatagonian Batholith
dc.subjectmagmatic rocks
dc.subjecthornfels
dc.subjectTierra del Fuego
dc.titleThe Magmatic Rocks Probably Corresponding to the Andean Batholith and the Associated Metamorphic Contact Phenomena
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeinfo:eu-repo/semantics/bookPart
dc.typeinfo:ar-repo/semantics/parte de libro


Este ítem pertenece a la siguiente institución