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Martín Turienzo,Luis Dimieri,Cristina Frisicale,Vanesa Araujo,Natalia Sanchéz
Pág. 317 - 357
In the Argentinean side of the Andes at 34°40?S, the Cenozoic Andean orogeny produced the thick-skinnedMalargüe fold-and-thrust belt and the easternmost basement uplift of the Cordillera Frontal. Integrating balanced structuralcross-sections with previou...
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