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Alternating contraction and extension in the Southern Central Andes (35°–37°S) | American Journal of Science
Neogene evolution of the Aconcagua fold-and-thrust belt: Linking structural, sedimentary analyses and provenance U-Pb detrital zircon data for the Penitentes basin - ScienceDirect
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Main folding structures in the folds zone of the thin-skinned central... | Download Scientific Diagram
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Mesozoic to Cenozoic retroarc basin evolution during changes in tectonic regime, southern Central Andes (31–33°S): Insights from zircon U-Pb geochronology - ScienceDirect
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