Strain partitioning along the arc in the Neuquén Andes (36-39°S) for the last 30 million years

The Neuquén Andes between 36 and 39°S were built by a broad range of processes during the last 30 Ma. Periods of deformation can be classified in two alternating types: periods of extension associated with homogeneous shear parallel to the trench, whose strain encompassed areas hundreds of kilometer...

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Detalles Bibliográficos
Autores principales:	Folguera, A., Ramos, V.A., Melnick, D.
Formato:	JOUR
Materias:	Northern Patagonian Andes Oblique subduction Strain partitioning Volcanic arc Wadati-Benioff changes Cenozoic crustal evolution strain partitioning subduction zone volcanism Andes Argentina Neuquen South America
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_07160208_v29_n2_p_Folguera
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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