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Chemical geothermometry and geobarometry in hydrothermal aqueous solutions: A theoretical investigation based on a mineral-solution equilibrium model

Journal Article · · Geochimica et Cosmochimica Acta; (United States)
 [1];  [2]; ;  [3]
  1. Univ. di Perugia (Italy)
  2. Ist. di Geocronologia, Pisa (Italy)
  3. Geotermica Italiana srl, Pisa (Italy)
The theoretical compositions of an aqueous solution in equilibrium with a mineral assemblage made up of low-albite, K-feldspar, either a Ca-Al-silicate or calcite, clinochlore, muscovite, quartz, anhydrite, and fluorite, under varying T-P{sub CO{sub 2}}-m{sub Cl} conditions of geothermal interest, indicate that (1) the total SO{sub 4} content as well as the Na/K,K{sup 2}/Mg, and SO{sub 4}/F{sup 2} ratios are potential geothermometers; (2) the total HCO{sub 3} content as well as the K{sup 2}/Ca,Ca/Mg, HCO{sub 3}/F, and (HCO{sub 3}){sup 2}/SO{sub 4} ratios are potential P{sub CO{sub 2}} indicators; (3) the Na, K, Ca, and Mg total contents as well as the Na{sup 2}/Mg and Na{sup 2}/Ca ratios are mainly controlled by the total ionic salinity and are therefore hardly suitable as geoindicators. A preliminary test of the equations involving total HCO{sub 3} content as well a K{sup 2}/Ca and HCO{sub 3}/F ratios as P{sub CO{sub 2}} indicators have provided satisfactory results.
OSTI ID:
7051630
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Journal Name: Geochimica et Cosmochimica Acta; (United States) Vol. 55:10; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English