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Basement evolution of the Sierra de la Ventana Fold Belt : new evidence for Cambrian continental rifting along the southern margin of Gondwana

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dc.contributor.authorRapela, Carlos Washington
dc.contributor.authorPankhurst, Robert John
dc.contributor.authorFanning, Christopher Mark
dc.contributor.authorGrecco, Laura E.
dc.date.issued2003
dc.descriptionFil: Rapela, Carlos Washington. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina.|Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET); Argentina.
dc.descriptionFil: Pankhurst, Robert John. Natural Environment Research Council (NERC); Reino Unido.
dc.descriptionFil: Fanning, Christopher Mark. Australian National University; Australia.
dc.descriptionFil: Grecco, Laura E.. Universidad Nacional del Sur; Argentina.
dc.descriptionUb: R9 335. Ej: 1. SALA.
dc.identifier002991
dc.identifier.urihttps://naturalis.fcnym.unlp.edu.ar/handle/628872547/42302
dc.languageeng
dc.sourceJournal of the Geological Society. 2003;160:613-628
dc.subjectGEOLOGIA
dc.subjectU-Pb SHRIMP
dc.subjectGondwana
dc.subjectGeochronology
dc.subjectGranites
dc.subjectRifting
dc.titleBasement evolution of the Sierra de la Ventana Fold Belt : new evidence for Cambrian continental rifting along the southern margin of Gondwana
dc.typeArtículo
dspace.entity.typePublication
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