Temporal variability of secondary processes in alkaline geothermal waters associated to granitic rocks: the Caldes de Boí geothermal system (Spain)
The Caldes de Boí geothermal waters show important differences in pH (6.5–9.6) and temperature (15.9ºC–52ºC) despite they have a common origin and a very simple circuit at depth (4km below the recharge area level). These differences are the result of secondary processes such as conductive cooling,...
-д хадгалсан:
| -д хэвлэсэн: | Geologica Acta: an international earth science journal |
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| Үндсэн зохиолчид: | , , , , , , |
| Формат: | Artigo |
| Хэл сонгох: | Inglês |
| Хэвлэсэн: |
Universitat de Barcelona
2017
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| Нөхцлүүд: | |
| Онлайн хандалт: | https://www.redalyc.org/articulo.oa?id=50551303001 https://www.redalyc.org/journal/505/50551303001/ https://www.redalyc.org/journal/505/50551303001/html/ https://www.redalyc.org/journal/505/50551303001/50551303001.epub https://www.redalyc.org/journal/505/50551303001/movil |
| Шошгууд: |
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