Evolution of Los Venados (San Luis, Argentina) during late Cenozoic
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Abstract
After analyzing the different morphological trends present in the range and their relationship with neotectonic structures, the evolution of the landscape is interpreted in relation to fault movements. The main faulting activity has been attributed to Middle Miocene -Pleistocene.
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How to Cite
Costa, C.H. , trans. 1991. “Evolution of Los Venados (San Luis, Argentina) During Late Cenozoic”. Alpine and Mediterranean Quaternary 4 (1a): 41-48. https://doi.org/10.26382/.
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