Structural evolution of the transition zone between the Aconcagua and Malargûe fold and thrust belts, province of Mendoza

In this work we describe briefly the stratigraphy and the structure of the Andes in the transition zone between the Aconcagua and Malargüe fold and thrust belts. The outcrops are a Permotriasic volcanic acid basement, Mesozoic sediments of the Cuenca Neuquina and Neogene volcanic rocks and continent...

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Autores principales: Broens, S., Pereira, D.M.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p685_Broens
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