References
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Heat flow study in ASCOPE countries as a follow-up to the first workshop
Metodika I Rezultaty Op-Redeleniya Teplovykh Potokov Na Ukrainskom Shchite I Ego Sklonakh (Methodology and Results of Heat Flux Determination on the Ukrainian Shield and its Slopes )
Electrical resistivity, sound velocity, thermal conductivity, density-porosity, and temperature, obtained by laboratory techniques and well logs: D site 462 in the Naru Basin of hte Pacific Ocean
Revised heat flow map of Colorado
Thermal regime of the Escalante Desert, Utah, with an analysis of the Newcastle geothermal system
Teplovoy Potok V Predelakh Zapadno-sibir- Skoy Plity (Heat flow within the Western Siberian Plate )
The geothermal hydrology of Warner Valley, Oregon - a reconnaissance study
Heat flow from the crust of the United States
Thermal and tectonic implications of heat flow in the Eastern Snake River Plain, Idaho
Heat flow from five uranium test wells in west-central Arizona
Heat flow from five uranium test wells in west-central Arizona
Heat‐flow determination in three DSDP boreholes near the Japan Trench
Geothermal potential of West-Central New Mexico from geochemical and thermal gradient data
To study the low temperature and Hot Dry Rock (HDR) geothermal potential of west-central New Mexico, 46 water samples were collected and geothermal gradient measurements were made in 29 wells. Water chemistry data indicate that all the samples collected are meteoric waters. High temperatures of samples taken from wells between Gallup and Tohatchi indicate these wells may derive water from a warm aquifer below the depth of the wells. The chemistries of the samples farther south on the Zuni Indian reservation suggest these waters are not circulating below 600 m of the surface. Geothermometry calculations support the conclusion that the …
ESTIMATION OF HEAT FLOW IN OIL WELLS BASED ON A RELATION BETWEEN HEAT CONDUCTIVITY AND SOUND VELOCITY
Heat flow from the Liberian Precambrian Shield
Uncorrected heat flow in iron formation rocks from three areas within the Liberian part of the West African Shield ranges from 50 to more than 80 mW m?2. When corrections are applied for topography and refraction, the range of heat flow is narrowed to between 38 and 42 mW m?2. In comparison with heat flows from other parts of the West African Craton, these values are consistent with preliminary results from Ghana (42±8 mW m?2) and Nigeria (38±2 mW m?2) but are somewhat higher than values from Niger (20 mW m?2) and neighboring Sierra Leone (26 mW m?2). The Liberian …