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...
Spremljeno u:
| Izdano u: | Andean Geology |
|---|---|
| Glavni autori: | , , |
| Format: | Artigo |
| Jezik: | Inglês |
| Izdano: |
Servicio Nacional de Geología y Minería
2013
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| Teme: | |
| Online pristup: | https://www.redalyc.org/articulo.oa?id=173925397006 |
| Oznake: |
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