References
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Bericht über geothermische Messungen in der Bohrung Böß-Gesäß
Heat flow measurements in the Ionian Sea with a new heat flow probe
Shallow Water Heat Flow Measurements in Bras D'or Lake, Nova Scotia
A light-weight oceanic thermal gradient probe was used for heat flow studies in Bras d'Or Lake, Nova Scotia. The measurements were made in St. Andrew's Channel, an elongated trough 270 m deep and 540 m wide. The heat flux of 1.50 μcal/cm2 s (63 mW/m2) is corrected for sedimentation, conductivity contrast, topography, and surface temperature differences.
Bestimmungen der terrestrischen Wärmestromdichte in Deutschland
O teplofizicheskikh svoystvakh gornykh porod nekotorykh rayonov Zapadnogoi Yuzhnogo Tyan'-Shanya i geotermicheskikh usloviyakh Ferganskoy vpadiny (On the thermophysical properties of rocks in some areas of the Western and the Southern Tien Shan and the geothermal conditions of the Fergana depression)
Reykjanes ridge crest: A detailed geophysical study
Heat flow and geothermal resource estimates for the Imperial Valley in Rex RW, principal investigator, Cooperative geological-geophysical-geochemical investigation oJ geothermal resources in the Imperial Valley oJ CaliJornia
Heat flow near major strike-slip faults in California
Heat flow, heat generation and crustal temperatures in the Kapuskasing area of the Canadian shield
Combined heat flow and heat production measurements in three boreholes in the Superior Province of the Canadian Shield were made to test the geothermal consequences of the Kapuskasing fault zone. The evidence of gravity and geomagnetic investigation suggests that this zone is a deeply eroded remnant of a crustal rift. A linear relation between heat flow (q) and surface heat production (P), q = qo + bP, where qo and b are empirical constants, has been found by F. Birch, R. Roy and A. Lachenbruch for different heat-flow provinces over the North American continent. The results from the Kapuskasing zone …
Heat flow measurements and a first heat flow map of Germany
Sediment transport and distribution in the Argentine Basin. 1. Antarctic Bottom Current passage through the Falkland fracture zone
Teplovoe Pole Ukrainy (Thermal Field of Ukraine)
Novye dannye o teplovom potoke cherez dno Indijskogo i Tihogo okeanov (New data on heat flow through the floors of the Indian and Pacific Oceans )
Terrestrial heat flow in Hokuriku district, central Japan
New data on heat flow through the floors of the Indian and Pacific Oceans
Novi Dani Pro Teplovii Potik Ukrains-Kogo Shchita (New Data About the Heat Flow of the Ukrainian Shield )
Terrestrial heat flow in deep borehole Zarosice 1 and 2 in the Zdanicke Forest region Zemsky tepelny tok v hlubinnych vrtech Zarosice-1 A 2 v oblasti zdanickeho lesa
Teplovoj potok nekotoryh rajonov Altae-Sajanskoj oblasti (Heat flow of some areas of the Altai-Sayan region )
Geothermal potential of Idaho. Review with 70 references
Uniform heat flow in a deep hole in the Canadian Shield and its paleoclimatic implications
Precise temperature measurements to 2865 meters in a hole in a granitic pluton near FHn Flon, Manitoba, Canada, showed a systematic increase of temperature gradient with depth. Conductivity determinations at 50-meter intervals revealed a corresponding systematic decrease in conductivity. Over the entire measured depth, no systematic deviation from the mean heat flow of 1.01±0.04 ?cal/cm2 sec is detectable in spite of strong evidence that the ground-surface temperature was at least 3.5°C cooler than at present for long periods during the Pleistocene epoch. These results can be reconciled with plausible paleoclimatic models. Evidently climatic change at this site does not result …