References
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Heat flow study along the iv ggt china
Pervye ocenki teplovogo potoka v Severnom Vietname (First estimates of the heat flow in North Vietnam )
Heat flow on the Qinghai-Xizang (Tibetan) Plateau and the modeling of the tectono-thermal evolution
Geothermal studies in Siberia and Mongolia
The first group of heat flow data in ganshu
Heat flow and subsurface temperature as evidence for basin-scale ground-water flow, North Slope of Alaska
Heat flow and thermal history of the exmouth plateau
Heat flow and tectonics of the Western Ross Sea
Heat flow, thermal structure and thermal evolution of the Paraná basin, Southern Brazil
Influence of terrain on bedrock temperatures
Tectonic and thermal structure of the Middle Valley sedimented rift, northern Juan de Fuca Ridge
Terrestrial heat flow and the thermal structure of the lithosphere in south Liaoning
Heat-Flow and Fluid-Flow Regime in the Western Nankai Accretionary Prism
The thermal structure of the western Nankai subduction zone has been studied through surface heat flow measurements with conventional geothermal probes and estimation of heat flow from depths of gas hydrate bottom simulating reflectors. Temperature and thermal conductivity measurements at ODP Site 808, located at the toe of the Nankai accretionary prism, added important information on any variation in heat flow with depth and thus on thermal effects of pore fluid flow in the prism. Surface heat flow is generally higher than 130 mW/m2 on the floor of the Nankai Trough. Such high heat flow cannot be explained simply by …
Heat flow in the south of the Nova-Canton Trough, central equatorial Pacific (GH82-4 Area)
Geothermal measuremetns: thermal evolution of the Japan Sea basins and sediments
Heat flow measurements around the Japanese Islands: Interpretation with reference to the tectonics in the Okinawa Trough (in Japanese)
Report on the first batch of measured geothermal flow data in Jiangxi Province
Heat flow measurements in Southeast China
Teplovoj potok cherez dno ozera Hubsugul i prilegajushhie gory (Mongolija) (Heat flow through the bottom of Khubsugul Lake and the bordering mountains (Mongolia) )
Heat flow in the sediments of lake rotorua
A total of 48 heat flow measurements were made in the sediments at the bottom of Lake Rotorua during June 1990. High heat flows (greater than 0.25 W/m2) were measured in the south-eastern part of the lake, and the total natural heat output for this area is estimated to be 20 MW. Within this area there are two regions with heat flow greater than 2 W/m2; one immediately north of Rotorua, and the other located between Mokoia Island and Rotokawa. The former marks the northward extension of the Rotorua geothermal field beneath the lake. The latter probably represents a separate …