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Hydrothermal alteration at Roosevelt Hot Springs KGRA - DDH 1976-1

Technical Report ·
DOI:https://doi.org/10.2172/5984607· OSTI ID:5984607
Hot waters of the Roosevelt Thermal Area, Utah, have altered granitic rocks and detritus of the Mineral Range pluton, Utah. Petrographic, x-ray, and chemical methods were used to characterize systematic changes in chemistry and mineralogy. Major alteration zones include: 1) an advanced argillic zone in the upper 30 feet of altered detritus containing alunite, opal, vermiculite, and relic quartz; 2) an argillic zone from 30 feet to 105 feet containing kaolinite, muscovite, and minor alunite; and 3) a propylitic zone from 105 to 200 feet containing muscovite, pyrite, marcasite, montmorillonite, and chlorite in weakly altered quartz monzonite. Comparison of the alternation mineral assemblages with known water chemistry and equilibrium activity diagrams suggests that a simple solution equilibrium model cannot account for the alteration. A model is proposed in which upward moving thermal water supersaturated with respect to quartz and a downward moving cool water undersaturated with respect to quartz produces the observed alteration. An estimate of the heat flow contributions from hydrothermal alteration was made by calculating reaction enthalpies for alteration reactions at each depth.
Research Organization:
Utah Univ., Salt Lake City (USA). Dept. of Geology and Geophysics
DOE Contract Number:
AS07-76ID01601
OSTI ID:
5984607
Report Number(s):
DOE/ID/01601-T9; ON: DE82003934
Country of Publication:
United States
Language:
English