References
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Rezultaty izucheniya teplofizicheskikh svoistv gornykh porod dlya tselei geologicheskogo kartirovaniya - v kn: primenenie geotermii v regionalnykh i poiskovo-razvedochnykh issledovaniyakh (Results of studying the thermophysical properties of rocks for the purposes of geological mapping - in the book: Application of geothermal energy in regional and prospecting and exploration studies)
Temperature profiles from Salt Valley, Utah, thermal conductivity of 10 samples from drill hole DOE 3, and preliminary estimates of heat flow
Geothermal conditions of Hungary
Estimates of the thermal state of the Arabian plate from heat flow, uplift, and volcanism of Western Saudi Arabia
Teplovoy potok i temperatura nedr osnovnykh geostructur kriolitozony SSSR (Heat flow and subsoil temperature of the main geostructures of the permafrost zone of the USSR
Heat flow and heat production from the Malingsbo granite, central Sweden
Heat transfer and intraplate deformation in the central Indian Ocean
Heat flow through the San Jacinto fault zone, southern California
Gerotermika zloza rud miedzi monokliny przedsudeckiej
Heat flow measurements in Lutzow-Holm bay, Antarctica-A Preliminary study
Water movement within lac du bonnet batholith as revealed by detailed thermal studies of three closely-spaced boreholes
Successive temperature logs have been obtained over a period of two years in three closely-spaced boreholes in the Lac du Bonnet batholith of the Superior Province of the Canadian Shield. Two of the boreholes, of depth 450 m and 830 m, intersect a dipping fracture zone at 435–450 m. In both holes water is flowing from near the surface to the fracture zone at approximately 1.5–1.9·10−5 m3 s−1, the flow being inferred from analysis of the temperature logs. Below 25 m, temperatures in these two holes are 0.22–0.28 K lower than those in the third, 145 m, hole. The temperature …
Severnyy Ledovityy Okean (Arctic Ocean)
Teplovoj potok v Barencevo-morskom regione (Heat flow in the Barents Sea region )
Geothermal studies in the San Juan Basin and the Four Corners area of the Colorado Plateau I. Terrestrial heat-flow measurements
Twenty-five new heat-flow measurements are presented for the San Juan Basin and the Four Corners area of the Colorado Plateau in the southwestern United States. Temperature gradients at most sites are calculated from temperature logs at depths between 1 km and 2 km. Resulting heat-flow values appear to be locally less variable than shallower data. These new data develop smooth, uniform trends consistent with the regional geology. As such, it is reasonable to suggest that these data may be somewhat less influenced by near surface perturbations to heat flow than are shallower data in the area; i.e., local hydrologie movement, …