dc.creatorDalla Salda, Luis Hugo
dc.creatorCingolani, Carlos Alberto
dc.creatorVarela, Ricardo
dc.date1992
dc.date2022-06-08T13:52:43Z
dc.date.accessioned2023-07-15T05:01:21Z
dc.date.available2023-07-15T05:01:21Z
dc.identifierhttp://sedici.unlp.edu.ar/handle/10915/137526
dc.identifierissn:0091-7613
dc.identifierissn:1943-2682
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/7471786
dc.descriptionThe late Precambrian to early Paleozoic age rock units of the Pampean ranges, the Puna, and the North Patagonian massif of southwestern South America constitute the Famatinian orogenic belt. They are interpreted as an Ordovician collisional belt between the Occidentalia terrane and the Gondwana craton. They include mafic and ultramafic belts of Neoproterozoic to early Paleozoic age. An intense tectonothermal event resulted from the collision; syntectonic granitoids represent crustal melting. In that collision syntectonic to late-tectonic foreland basins developed. The recently proposed juxtaposition of Laurentia and East Antarctica-Australia in the Neoproterozoic raises the possibility that Laurentia and western South America were close together in the early Paleozoic, and therefore that the Famatinian belt resulted from Laurentia-Gondwana collision. Occidentalia, which is bordered by a Cambrian carbonate platform similar to that of eastern North America, may be a sliver detached from Laurentia during Late Ordovician time.
dc.descriptionFacultad de Ciencias Naturales y Museo
dc.formatapplication/pdf
dc.format617-620
dc.languageen
dc.rightshttp://creativecommons.org/licenses/by-nc-sa/4.0/
dc.rightsCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
dc.subjectGeología
dc.subjectEarly Paleozoic
dc.subjectSouth America
dc.subjectOrdovician collisional belt
dc.titleEarly Paleozoic orogenic belt of the Andes in southwestern South America: result of Laurentia-Gondwana collision?
dc.typeArticulo
dc.typeArticulo


Este ítem pertenece a la siguiente institución