BASALTIC EXPLOSIVE VOLCANISM IN A TUFF-DOMINATED INTRAPLATE SETTING, SARMIENTO FORMATION (MIDDLE EOCENE- LOWER MIOCENE), PATAGONIA ARGENTINA
The Sarmiento Formation (middle Eocene to early Miocene) represents the distal recordof the activity of the Andean volcanic arc in central Patagonia, mainly dominated by accumulationand reworking of fine ash in a low-gradient continental setting. Intraplate volcanism takes place inthe Golfo San Jorg...
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| Vydáno v: | Latin American Journal of Sedimentology and Basin Analysis |
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| Hlavní autoři: | , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Asociación Argentina de Sedimentología
2008
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=381740362001 |
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