References
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Informativnost' geotermii pri izuchenii zemnoj kory Ural'skoj evgeosinklinali (Informative value of geothermy in the study of the earth's crust of the Ural eugeosyncline )
Heat flow in Indian Gondwana basins and heat production in basement rocks
Premières déterminations du flux de chaleur et de la production de chaleur en Corse
Assessment of geothermal resources of Brazil — 1981
Thermal ground water flow systems in the thrust zone in southeastern Idaho
Regional Geothermal Exploration in Egypt
Abstract Although Egypt is not characterized by abundant Cenozoic igneous activity, its location in the northeastern corner of the African plate suggests that it may possess geothermal resources, especially along its eastern margin. Regional geothermal exploration has been carried out in Egypt using the thermal gradient/heat flow technique and groundwater temperature/chemistry technique. In the thermal gradient/heat flow study, existing oil-well bottom-hole temperature data as well as subsurface temperature measurements in existing boreholes were utilized before special thermal gradient holes were drilled. Groundwater temperature and chemistry data were used to extend the geographic range of the direct subsurface thermal measurements. On …
Geothermal low-temperature reservoir assessment in Dona Ana County, New Mexico. Final report
Heat flow on the western flank of the East Pacific Rise at 21°N
Metodika i rezul'taty opredeleniya teplovogo potoka v zone sochleneniya dokembrijskoj Vostochno-Evropejskoj i paleozojskoj Zapadno-Sibirskoj platform (The methods and results of a heat flow determination in the junction zone of the Precambrian East European and Paleozoic West Siberian Platforms )
Initial Reports of the Deep Sea Drilling Project
Heat transfer through the sediments of the Mounds Hydrothermal Area, Galapagos Spreading Center at 86°W
Geotermicheskie Usloviya Uchastka Shakhty Arpa-Sevan (Geothermal conditions of the Arpa-Sevan mine site )
On the terrestrial heat flow and physical limnology of Crater Lake, Oregon
The heat flow into 7000-year-old Crater Lake caldera is dominated by hydrothermal processes. The average of the conducted heat flow value is 138±121 mW/m2 (3.3±2.9 HFU). The total heat flow is estimated to be between 669 and 1381 mW/m2 (16 and 33 HFU). Hydrothermal fluids penetrate into the lake floor to a depth of at least 1.5 to 2.0 km and possibly much deeper. Two thermal spring areas were discovered on the deep lake floor. These springs, and probably other as yet undiscovered ones, have a dramatic effect on the water temperature, circulation, and stratification of the lake. Dense thermal …