| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 10687604 | Geothermics | 2005 | 23 Pages |
Abstract
The thermal springs of Na-Cl to Na-Cl-HCO3 type located in the Chachimbiro area originate through dilution of the parent geothermal water and have reached different degrees of re-equilibration with country rocks at lower temperatures.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Eduardo Aguilera, Roberto Cioni, Fabrizio Gherardi, Gabriella Magro, Luigi Marini, Zhonghe Pang,