Meager Creek Geothermal Project: an exploration case history
The South Reservoir in the Meager Creek Geothermal Area is within crystalline basement rocks on the southern flank of the Pliocene to Recent Meager Mountain Volcanic Complex. Geological, geochemical and resistivity surveys were used to determine targets for temperature gradient diamond drilling. Temperature profiles indicate anomalously high temperature gradients in drill holes M2, M3, M4, M6, M7, M8, M10, M11, and M12. Heat flow values of 105 to 620 mWm/sup -2/ (2.5 to 14.8 HFU) have been calculated for drill holes M2, M3, M7, M8, M11 and M12. These values are up to seven times the regional heat flow for the Garibaldi Volcanic Belt. The main South Reservoir thermal anomaly has been defined over an area about 3 km by 1 km in the Meager Creek valley. The anomaly is open to the north and southeast.
- OSTI ID:
- 5745243
- Journal Information:
- Bull., Geotherm. Resour. Counc. (Davis, Calif.); (United States), Vol. 10:6
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
CANADA
GEOTHERMAL RESOURCES
GEOCHEMICAL SURVEYS
GEOLOGIC MODELS
GEOLOGY
GEOTHERMAL EXPLORATION
HEAT FLOW
RESISTIVITY SURVEYS
WELL DRILLING
DRILLING
ELECTRICAL SURVEYS
EXPLORATION
GEOPHYSICAL SURVEYS
NORTH AMERICA
RESOURCES
SURVEYS
150300* - Geothermal Exploration & Exploration Technology
150202 - Geology & Hydrology of Geothermal Systems- Non-USA- (-1989)