References
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Heat flow on the south flank of the Snake River rift (abs.)
Heat flow in the Mariana Marginal Basin
No-Vye Opredeleniya Teplovogo Potoka V Karpatskom Regione (New Heat Flow Determination in the Carpathian Region )
Izmerenie Teplovykh Po-Tokov Na Territorii Yugo-Zapada Vostochno-Evropeiskoi Platformy (Measuring Heat Flows in the Southwest Territory of the East European Platform )
Terrestrial heat flow determinations from lakes in southern Norway
Geotermicheskoe pole Bajkal'skoj riftovoj zony i sopredel'nyh rajonov (Geothermal field of the Baikal rift zone and adjacent areas )
Teplovoj potok v pos Listvennichnoe na poberezh'e Bajkala (Heat flow in the Listvennichnoe on the coast of Lake Baikal )
Pervye Dannye Po Izucheniyu TeplovykhPotokov Cherez Dno Kaspiiskogo Morya (First Data on the Study of Heat Flows across the Caspian Sea Bottom )
Rozklad pola cieplnegoziemi na obszare Polski Problem Wezlowy 01.1.1 N/.3 (in Polish)
Heat-flow near a North Atlantic fracture zone
Fifteen new heat-flow measurements are reported, fourteen of which are located in or near a fracture zone near 43°N on the mid-Atlantic Ridge. These data, combined with earlier nearby measurements, show the fracture zone to have an observable, positive effect on the regional heat-flow field. A good correlation is observed between large near-bottom water potential temperature gradients and the occurrence of significant variations with depth in the measured rate of heat-flow. One measurement was taken in the Horseshoe abyssal plain west of Gibraltar and gave a value of 1.38 μcal/cm2s.
Heat flow and thermal conductivity measurements, Leg 25, Deep Sea Drilling Project
Terrestrial heat flow measurements near rosignano solvay (Tuscany), Italy
Heat flow and heat production in northeast Africa
Enviromnetal and geophysical interpreation of heat-flow measurements in the Black Sea
The observed mean of 16 reliable heat-flow values in the Black Sea is 0.92 ± 0.23 μcal/cm2/sec. The observed heat flow is about 50 percent of the geophysically relevant heat flow because the rapidly accumulating sediment absorbs a significant fraction of the geothermal flux. In addition, the blanketing effect of the thick low-thermal-conductivity sediments in the Black Sea has further reduced the flux through the seafloor by about 15 percent. The mean heat flux out of the Black Sea, corrected for both thermal refraction and sedimentation, is estimated at 2.2 μcal/cm2/sec. The value of heat flowing into the base of …