Late Cretaceous Uplift in the Malargüe fold-and-thrust belt (35°S), southern Central Andes of Argentina and Chile
The Cordillera de los Andes is the typical example of a subduction-related orogen. Its present topography is the result of post-Miocene uplift, however, Andean compressional deformation and uplift started in the Late Cretaceous, as increasingly recognized in different sectors of the mountain belt. W...
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| Опубликовано в:: | Andean Geology |
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| Главные авторы: | , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Servicio Nacional de Geología y Minería
2013
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| Предметы: | |
| Online-ссылка: | https://www.redalyc.org/articulo.oa?id=173925397006 |
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