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Isotopic Analysis At Clear Lake Area (Thompson, Et Al., 1992)
ExplorationOutcome useful  +
ExplorationTechnique Isotopic Analysis- Fluid +
Notes Deuterium and oxygen- 18 values of the the
Deuterium and oxygen- 18 values of the thermal waters indicate that they recharged locally and became K271enriched in oxygen-18 by exchange with rock. The isotopic composition of the waters indicates that they are of meteoric origin. A plot of deuterium versus chloride indicates that as the chloride concentration increases, the deuterium composition remains essentially constant. A plot of oxygen-18 versus chloride shows that the oxygen isotopes become more enriched as the chloride concentration increases. Tritium data are consistent with the presence of two water types and show that the waters are little mixed because no intermediate tritium values are present.
o intermediate tritium values are present.  +
OpenEI/PageDescription Isotopic Analysis At Clear Lake Area (Thompson, Et Al., 1992): geothermal exploration activity.  +
OpenEI/PageKeyword Geothermal  + , Clear Lake Area  + , Isotopic Analysis- Fluid  +
Place Clear Lake Area +
Reference material Thermal Waters Along The Konocti Bay Fault Zone, Lake County, California- A Re-Evaluation +
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Isotopic Analysis At Clear Lake Area (Thompson, Et Al., 1992) + , Isotopic Analysis At Clear Lake Area (Thompson, Et Al., 1992) +
Categories Geothermal , Exploration Activities
Modification date
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17:05:20, 7 October 2013  +
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Isotopic Analysis (Rock, Fluid & Gas) At Clear Lake Area (Thompson, Et Al., 1992) + redirect page
 
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