Teleseismic-Seismic Monitoring
From Open Energy Information
GEOTHERMAL ENERGYGeothermal Home
Exploration Technique: Teleseismic-Seismic Monitoring
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| Exploration Technique Information | |
|---|---|
| Exploration Group: | Geophysical Techniques |
| Exploration Sub Group: | Seismic Techniques |
| Parent Exploration Technique: | Passive Seismic Techniques |
| Information Provided by Technique | |
| Lithology: | Rock unit density influences elastic wave velocities. |
| Stratigraphic/Structural: | Map geothermal reservoir geometry. Structural geology- faults, folds, grabens, horst blocks, sedimentary layering, discontinuities, etc. |
| Hydrological: | Combining compressional and shear wave results can indicate the presence of fluid saturation in the formation. |
| Thermal: | High temperatures and pressure impact the compressional and shear wave velocities. |
- Unspecified
- Central Nevada Seismic Zone Geothermal Region
- Clear Lake Geothermal Area
- Coso Geothermal Area
- Geysers Geothermal Area
- Hawthorne Geothermal Area
- Kilauea Southwest Rift And South Flank Geothermal Area
- Kilauea Summit Geothermal Area
- Lassen Volcanic National Park Geothermal Area
- Long Valley Caldera Geothermal Area
- New River Geothermal Area
- Newberry Caldera Geothermal Area
- Northern Basin and Range Geothermal Region
- Northwest Basin and Range Geothermal Region
- Valles Caldera - Redondo Geothermal Area
- Valles Caldera - Sulphur Springs Geothermal Area
- Walker-Lane Transition Zone Geothermal Region
- Yellowstone Caldera Geothermal Region