Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5779235 | Procedia Earth and Planetary Science | 2017 | 4 Pages |
Abstract
The reservoir temperature of the waters in the low temperature carbonate-evaporitic geothermal system of Arnedillo has been estimated by using two different techniques: 1) chemical geothermometers and 2) geothermometrical modelling. By combining the results of both techniques a reliable range of temperature of 90 ± 20°C has been proposed for the waters in the reservoir. Despite being a carbonate-evaporitic system, the cationic geothermometers have provided good results, which, together with the geothermometrical modelling, indicate that the waters have reached equilibrium with anhydrite, quartz, calcite, dolomite, albite and K-feldspar in the reservoir.
Keywords
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Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
Mónica Blasco, Luis F. Auqué, MarÃa J. Gimeno,