References
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EARLY SUBSURFACE TEMPERATURE MEASUREMENTS IN THE NETHERLANDS
Geotermicheskie issledovanija SahKNII v severo-zapadnom sektore Tihookeanskogo podvizhnogo pojasa (Geothermal research of the Sakhalin Research Institute in the north-western sector of the Pacific mobile belt )
Geotermicheskie osobennosti i merzlaja zona hr Suntar-Hajata (na primere Nezhdaninskogo mestorozhdenija) (Geothermal features and the frozen zone of the Suntar-Khayata Ridge Suntar-Khayata (by the example of the Nezhdaninskoye field) )
Rekonstrukcija paleoklimata po sovremennym geotermicheskim dannym (Reconstruction of paleoclimate from modern geothermal data )
Eine Wärmestromanomalie bei Freiberg
Heat flow of Oregon
Geotermicheskie issledovanija na ostrove Moneron (Geothermal exploration on Moneron Island )
Geotermicheskaya Kharakteristika Mestorozhdeniya Sytykan (Geothermal characteristics of the Sytykan deposit )
Heat fow, thermal conductivity, thermal gradient
On the geothermal regime of some tectonic units in Romania
Heat flow values of 33–58 mW m−2 were found for the Transylvanian Depression, 45–57 mW m−2 for the crystalline nucleus of the Eastern Carpathians, and 70–120 mW m−2 for the Neogene volcanic area. Temperature-depth profile and some geophysical implications of the low values for the Transylvanian Depression are discussed, rendering evident clear-cut differences between this tectonic unit and other Noegene depressions. The heat flow values for the other two investigated tectonic units are usual ones for areas of their age.
Downhole temperature measurements and heat flow data in the Black Sea — DSDP Leg 42B
Down-hole temperature measurements, Deep Sea Drilling Project, Leg 42A
Geophysical measurements in the region of the Explorer ridge off western Canada
GEOTHERMAL GRADIENTS IN THE SOUTHERN NIGERIA BASIN
Subsurface temperatures from the Southern Nigeria Basin obtained from the Nigerian Federal Ministry of Petroleum Resources were used in the determination of subsurface temperature gradients. Temperature measurements made with maximum recording thermometers were obtained from electric logs and production data. Fields without production temperature data had their temperatures corrected to true subsurface temperatures, using a 22 per cent correction factor.Temperature gradients in the Niger Delta range from 1.20 to 3.00°F/100 ft (31 m) based on an average surface temperature intercept of 74°F. Maximum temperature gradients occur in the Anambra Basin with fairly high gradients in the offshore western and eastern …
Heat flow studies in the steamboat mountain-lemei rock area, Skamania County, Washington
Report of heat flow measurements in San Juan and Mendoza, Argentina
Report of Heat Flow Measurements in Chile
Crustal thermal models for South Siberia
The results of geothermal research carried out in South Siberia (West-Siberian and Siberian Platforms, Altai-Sayan folded area and the Baikalian arched uplift zone) were employed to calculate the Earth's crustal temperatures. It is shown that temperature is a function of the heat flow value. The maps of the surface heat flow and the temperatures at the Moho discontinuity are presented and characteristic temperature-depth profiles were compiled for specific tectonic areas. The West-Siberian and Siberian Platforms, as well as the Altai-Sayan folded region are characterized by rather low heat flow, 42–50mW m−2(1.0–1.2 µcal/cm2s), and low temperatures at the Moho boundary.400–500 °C. …