Helium determinations as an exploration technique at the Ambrosia Lake uranium district, McKinley County, New Mexico
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This report updates U.S. Geological Survey Open-File Report 77-780 by including new field data taken in July 1978. A revised geologic map is included, as are new geophysical data from an approximately 0.3-km by 0.5-km area just northeast of and adjoining the area surveyed earlier. The pattern which had been observed to the southwest of spatially coincident radiometric highs, magnetic highs, and resistivity lows deteriorates to the northeast: there the radiometric highs fall on magnetic lows and the correlation with resistivity lows disappears.
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As a sulfate-bearing, hydrothermal solution cools to less than about 200°C, kinetic factors prevent sulfate from entering into oxidation-reduction reactions. Consequently, the reducing effect of H 2 S (and other reduced species) is not balanced with the oxidizing effect of SO 4 = to the same extent as at higher temperatures. The result is a lower effective Eh of the system. This decrease in the effective Eh due to a slowing of the rate of sulfate reduction with cooling may be the precipitation mechanism for many types of ore deposits.