Application of different geothermometrical techniques to a low enthalpy thermal system

Blasco, M. (Universidad de Zaragoza) ; Auqué, L.F. (Universidad de Zaragoza) ; Gimeno, M.J. (Universidad de Zaragoza)
Application of different geothermometrical techniques to a low enthalpy thermal system
Resumen: 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 oC 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.
Idioma: Inglés
DOI: 10.1016/j.proeps.2016.12.034
Año: 2017
Publicado en: Procedia Earth and Planetary Sciences 17 (2017), 65-68
ISSN: 1878-5220

Financiación: info:eu-repo/grantAgreement/ES/MEC/FPU14-01523
Tipo y forma: Article (Published version)
Área (Departamento): Área Petrología y Geoquímica (Dpto. Ciencias de la Tierra)

Creative Commons You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use. You may not use the material for commercial purposes. If you remix, transform, or build upon the material, you may not distribute the modified material.


Exportado de SIDERAL (2023-01-11-10:04:06)


Visitas y descargas

Este artículo se encuentra en las siguientes colecciones:
Articles



 Record created 2017-02-01, last modified 2023-01-11


Versión publicada:
 PDF
Rate this document:

Rate this document:
1
2
3
 
(Not yet reviewed)