References

Heat flow and surface radioactivity measurements in the Precambrian Shield of Western Australia

Some heat-flow measurements in the North Atlantic Ocean

Gidro-geologicheskie I Geotermicheskie Uslovija Kurorta Tamisk (Severo-Osetinskaja Assr) (Hydro-geological and Geothermal Conditions of Tamisk Resort (North Ossetian Assr) )

Teplovoi potok po skvazhine kadzharan - 480 - doklady an arm ssr 1968 (Heat flow through the kajaran well )

Heat Flow measurements in a low Radioactivity area of the Western Australian Precambrian Shield

Heat flow data 2

The first comprehensive listing of heat flow data was made by Lee (1963) ; it was subsequently revised by Lee and Uyeda (1965) and Lee and Clark (1966). Several hundred additional heat flow values have since appeared in the literature. The data that have appeared since the compilation by Lee and Clark or that are now in press are tabulated in this report. To keep the tabulation of heat flow data current, we expect to present a semi-annual summary in the Journal of Geophysical Research or another publication of the American Geophysical Union.

Měřeni teploty a tepelný tok v přibramských dolech (Temperature and heat flow measurement in Přibram mines)

Terrestrial heat flow in the Bohemian Massif and its relation to the deep structure

Heat flow in the Zacler–Svatonovice basin

Three measurements of heat flow in eastern Canada

Terrestrial heat flow in Finland

Finland is part of an ancient, Precambrian area known as the Baltic Shield. During the years 1960–1966, geothermal measurements were carried out at five points in southern and central Finland. In conjunction with these investigations, 212 temperature measurements were made in drill holes and 106 thermal conductivity determinations from core samples. In the temperature measurements, a copper wire resistance or thermistor probe and a portable Wheatstone bridge were used. The thermal conductivities were measured by a steady-state comparison method very similar to that used by birch (1950). The average temperature gradients measured in the different drill holes vary within the …

Der Erdwärmefluss in der südwestlichen Slowakei

Termika Zemli i Luny (Earth’s and Moon’s thermal state )

Teplofizicheskie svojstva gornyh porod i velichina plotnosti teplovogo potoka po stvolu skvazhiny (Thermophysical property of rocks and the value of the density of heat flux along the borehole )

Geothermal data from the Vienna Basin

Relationship between terrestrial heat flow and the tectonics of continents

Měřeni tepelného toku ve dvou šachtách v západnich a jižnich Čechách (Heat flow measurements in mines of the western and southern Bohemia)

Terrestrial heat flow in eastern Slovakia

Heat Flow in the Sea of Japan

Summary Thirty-eight new heat flow values, obtained mainly in the western part of the Sea of Japan, are presented. Together with 117 earlier values, these measurements establish a generally high heat flow in that area. The heat flow values range from 1.28 to 5.33 ?cal/cm2 sec, and the average of 155 measurements is 2.22±0.53 (s.d.) ?cal/cm2 sec. Heat flow is very high in the northeastern basin and the westernmost plateau, while an east-west zone crossing Yamato rise has relatively low heat flow. The high heat flow in the Sea of Japan is tentatively thought to be caused by hidden volcanic …

Heat flow and surface radioactivity in the Quirke Lake Syncline near Elliot Lake, Ontario, Canada

Heat flow was measured in seven diamond-drilled holes, ranging in depth from 300 to 900 m, in the Quirke Lake Syncline (82° 30′ W, 46° 30′ N, mean elevation 370 m), Values for individual holes vary from 1.20 to 1.40 with a mean of 1.32 ± 0.02 μcal/cm2s, and no systematic variation was detected within the 50 km2 area studied. Radiometric measurements with a portable, three-channel, gamma-ray spectrometer show a downward concentration (stratigraphically) of Th, U, and K within the lower part of the syncline, with mean concentrations of 12.7 ppm, 3.3 ppm, and 1.9%, respectively. These data yield an …