Paper No. 93
Presentation Time: 8:00 AM


WHEELER, Joseph L., Earth Science and Geography, Vassar College, 124 Raymond Avenue, Poughkeepsie, NY 12604 and WALKER, Jeffrey R., Earth Science and Geography, Vassar College, 124 Raymond Ave, Box 735, Poughkeepsie, NY 12604,

The MH-2 hole was one of three holes completed as a part of HOTSPOT: The Continental Scientific Drilling Project. MH-2 was drilled to a depth of 1821m on the Mountain Home Air Force Base southeast of Boise, Idaho to evaluate the potential for development for geothermal energy on the base. Water under artesian pressure at a temperature of 140°C was encountered at a depth of 1745 m. We analyzed pieces of the core to study clay mineralization with depth. We took 22 samples from the bottom half of the core, focusing on the zone around 1790m, where preliminary analysis indicated the presence of corrensite (R1 ordered smectite/chlorite). X-ray diffraction (XRD) of these powders showed a transition from smectite at 762m to corrensite at 1790m and back to smectite at 1807m. More detailed XRD analysis with ethylene-glycol solvated samples confirmed the findings of the powder samples (namely a transition from smectite -> corrensite -> smectite). Samples around 1790m showed the presence of smectite, corrensite, and possibly chlorite (or serpentine). We modeled smectite and corrensite diffracting domain size with depth and found an increase in the defect-free distance of both minerals. We interpret this result to support a discontinuous (stepwise) model for the smectite-chlorite transition. The presence of warm artesian fluid in this zone is evidence for the importance of high fluid/rock ratios in the smectite-chlorite transition, and the association of high fluid/rock ratios with a discontinuous transition model.