Active sinking at the bottom of the Rincón de Parangueo Maar (Guanajuato, México) and its probable relation with subsidence faults at Salamanca and Celaya
Abstract Rincon de Parangueo is a Quaternary maar that had a perennial lake until the 1980s. The lake was gradually desiccated as a con - sequence of drawdown in the Salamanca-Valle de Santiago regional aquifer and now functions as a playa-lake. In contrast with the features observed in other crate...
Kaydedildi:
| Yayımlandı: | Boletín de la Sociedad Geológica Mexicana |
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| Asıl Yazarlar: | , , , , , , , , , , |
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Sociedad Geológica Mexicana, A.C.
2013
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| Konular: | |
| Online Erişim: | https://www.redalyc.org/articulo.oa?id=94348265014 |
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