Hydrological change during the Pleistocene-Holocene transition associated with the Last Glacial Maximum-Altithermal in the eastern border of northern Puna
The environment of the Andean Puna Plateau is mostly characterized by the dominance of evaporative processes due to aridity. Since the intermittent runoff lacks the morphodynamic competence to generate the present day landscape, authors have usually considered that the Puna landscape is a remnant fe...
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| Pubblicato in: | Andean Geology |
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| Autori principali: | , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Servicio Nacional de Geología y Minería
2015
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| Soggetti: | |
| Accesso online: | https://www.redalyc.org/articulo.oa?id=173936233001 |
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