Thick-skinned and thin-skinned thrusting in the La Ramada fold and thrust belt: Crustal evolution of the High Andes of San Juan, Argentina (32°SL)

The Cenozoic structural evolution of the La Ramada fold and thrust belt in the High Andes of Argentina, between 32°00'S and 32°30'S, shows in time and space the interaction of thin-skinned and thick-skinned deformations. Based on geometric and kinematic constraints, three different deforma...

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Autores principales: Cristallini, E.O., Ramos, V.A.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00401951_v317_n3-4_p205_Cristallini
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