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U.S. Department of Energy
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Hydrothermal alteration at the Roosevelt Hot Springs Thermal Area, Utah: petrographic characterization of the alteration to 2 kilometers depth

Technical Report ·
OSTI ID:6615273
Hydrothermal alteration in drill cuttings from Thermal Power drillhole 14-2, Roosevelt Hot Springs Thermal area, was studied petrographically. The hole is sited in alluvium approximately 1.6 km southeast of the old resort and was rotary drilled to a depth of 1866.0 m. Hydrothermal alteration has affected all rocks in the drillhole. Original rock textures are generally preserved. Significant changes in alteration mineralogy and intensity, which do not appear to be rock-type dependent, were observed. Alteration was described in three ways: pervasive alteration mineralogy was described by determining the alteration products of each of the major mineral species; vein and fracture fillings were described where recognized; and intensity of alteration was described by estimating the amount of destruction of major mineral species. Because of the nature of the samples (cuttings) the relationships of mineralogy and intensity to veins and fractures cannot be determined, but overall patterns clearly emerge. Mineral types identified include plagioclase, hornblende, biotite, sphene, and sulfides. (JGB)
Research Organization:
Utah Univ., Salt Lake City (USA). Dept. of Geology and Geophysics
OSTI ID:
6615273
Report Number(s):
IDO-78-170.a.1.1
Country of Publication:
United States
Language:
English