References
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Radioaktivnye jelementy i teplovoj potok zemnoj kory poluostrova Kamchatka (Radioactive elements and the heat flow of the earth's crust of the Kamchatka Peninsula )
Sub-surface temperatures from heat flow studies in the United Kingdom
Heat flow in the Hokkaido-Okhotsk region and its tectonic implications
Preliminary data of heat flow distribution in Romania
Heat flow values in 21 deep wells in various geological units of Romania were obtained. Some correlations among heat flow within the Moldavian platform (0·92–1·39 HFU), the Moesian platform (1·06–1·86 HFU) as well as the Carpathian folded chain (1·12–2·25 HFU) and structural features of these major units could be established.
Zona anomal'no nizkih teplovyh potokov na Yuzhnom Urale (An area of abnormally low heat flows in the Southern Urals )
Terrestrial heat flow in Edelény
Application of heat-flow techniques to geothermal energy exploration, leach hot springs area, grass valley, Nevada
Further data on the South-west England heat flow anomaly
Heat flow in the oceanic crust bounding Western Africa
Geothermal studies in Antarctica
Analysis of heat flow data—detailed observations in many holes in a small area
CU PRIVIRE LA REGIMUL GEOTERMIC AL UNITATILOR STRUCTURALE DE INTERES PENTRU HIDROCARBURI DIN ROMANIA (ON THE GEOTHERMAL CONDITIONS OF STRUCTURAL UNITS FOR ROMANIAN HYDROCARBONS)
Geothermal data from test wells drilled in Grass Valley and Buffalo Valley, Nevada
the geothermal potential evaluation of mexico by geothermal chemistry
Heat flow data and their relation to observed geothermal phenomena near Klamath Falls, Oregon
Heat flow data and their relation to observed geothermal phenomena near Klamath Falls, Oregon
Two holes were drilled to depths of about 180 m in the Lower Klamath Lake basin south of Klamath Falls, Oregon, to obtain heat flow data and to provide estimates of the thermal conductivity of the valley fill. Twenty-nine thermal conductivity determinations on eight cores give a mean conductivity of 1.82 mcal/cm s °C (0.75 W/m °K). Curvature in the upper 50 m of both terriperature profiles indicates a decrease in surface temperature of about 1.8°C, presumably resulting frorn reclamation of what was marshland in the early part of this century. A surprisingly low heat flow of 0.3 HFU (1 …
Heat flow near Kyle Hot Springs, Buena Vista Valley, Nevada
It is apparent that heat flow in the area of the electrical geophysical anomaly on the western flank of the East Range is not significantly higher than average for the ”Battle Mountain High,” and is typical of other values measured in bedrock in the region. Therefore it is unlikely that the anomalous zone is indicative of the presence of a hydrothermal system in that area.