Tectonic rotations in the Deseado Massif, southern Patagonia, during the breakup of Western Gondwana

Paleomagnetic investigation in the Deseado Massif, southern Patagonia, suggests that Triassic sedimentary rocks carry a latest Triassic to Jurassic remagnetization and that earliest Jurassic plutonic complexes carry a reversed polarity magnetization of thermoremanent origin. Despite uncertainties in...

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Detalles Bibliográficos
Autores principales:	Somoza, R., Vizán, H., Taylor, G.K.
Formato:	JOUR
Materias:	Gondwana breakup Jurassic Paleomagnetism Patagonia apparent polar wander path continental breakup crustal structure deformation Gondwana paleomagnetism remagnetization sedimentary rock tectonic evolution tectonic structure Triassic South America
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00401951_v460_n1-4_p178_Somoza
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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