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Geothermal resources of Wyoming sedimentary basins

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:6515912
Geothermal resources of Wyoming sedimentary basins have been defined through analysis of over 14,000 oil well bottom-hole temperatures, thermal logging of 380 wells, measurement of rock thermal conductivities, calculation of 60 heat-flow values, drilling of 9 geothermal exploratory wells, conductive thermal modeling, and the study of existing geologic, hydrologic, and thermal spring data. All data have been integrated into interpretations of the thermal structure of the Big Horn, Wind River, Washakie, Great Divide, Green River, Laramie, Hanna, and Shirley basins of Wyoming. Controlling factors for the formation of geothermal resources in these basins are regional heat flow, rock thermal conductivity values, depths to regional aquifers, and hydrologic flow directions. Regional basin heat-flow values range from about 40 to 80 milliwatts/m/sub 2/; measured thermal conductivities are in the general range of 1.5 to 4.0 watts/m/sup 0/K; and depths to aquifers are up to 11,000 m (36,000 ft). This results in regional geothermal gradients for Wyoming basins in the range of 15/sup 0/ to 40/sup 0/C/km (44/sup 0/ to 116/sup 0/F/mi) with predicted maximum aquifer temperatures near 300/sup 0/C (570/sup 0/F). Anomalous geothermal areas within the basins contain measured thermal gradients as high as 400/sup 0/C/km (1,160/sup 0/F/mi) over shallow depth intervals. These anomalous areas are the combined result of local geologic structures and hydrologic flow. A simplified model for such areas requires water movement through a syncline with subsequent heating due to regional heat flow and thermal conductivities of overlying rock units. Consequent flow of the heated water up over an anticline produces a localized area of anomalous geothermal gradients.
Research Organization:
Univ. of Wyoming, Laramie
OSTI ID:
6515912
Report Number(s):
CONF-8309274-
Conference Information:
Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 67:8
Country of Publication:
United States
Language:
English