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Compound and Elemental Analysis At Valles Caldera - Redondo Geothermal Area (White, Et Al., 1992)
ExpActivityDateEnd 1992  +
ExplorationOutcome not indicated  +
ExplorationTechnique Compound and Elemental Analysis +
Notes The study used various geochemical techniq
The study used various geochemical techniques to estimate fluid-rock mass transfer rates in reservoir rocks consisting primarily of Bandelier Tuff. Equilibrium constraints, fluid reservoir volume and discharge rates suggest that fluid residence time is approximately 2 _ 103 years, or <0.2% of the total age of the hydrothermal system. These results are suggestive of a geochemically and isotopically open system, in which Cl was the only aqueous component not controlled by mineral equilibrium.
ent not controlled by mineral equilibrium.  +
OpenEI/PageDescription Compound and Elemental Analysis At Valles Caldera - Redondo Geothermal Area (White, Et Al., 1992): geothermal exploration activity.  +
OpenEI/PageKeyword Geothermal  + , Valles Caldera - Redondo Geothermal Area  + , Compound and Elemental Analysis  +
Place Valles Caldera - Redondo Geothermal Area +
Reference material Mass Transfer Constraints On The Chemical Evolution Of An Active Hydrothermal System, Valles Caldera, New Mexico +
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Compound and Elemental Analysis At Valles Caldera - Redondo Geothermal Area (White, Et Al., 1992) + , Compound and Elemental Analysis At Valles Caldera - Redondo Geothermal Area (White, Et Al., 1992) +
Categories Geothermal , Exploration Activities
Modification date
"Modification date" is a predefined property that corresponds to the date of the last modification of a subject and is provided by Semantic MediaWiki.
16:03:57, 23 June 2014  +
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