References
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Teplovye Svoistva Porod (Thermal Properties of Rocks )
Caracteristic features of the heat flow profile on the continental margin in the northern part of south china sea and theri geological significance
Temperatures and depth dependent heat flow in western North Sea
Bottom-hole temperatures and lithologic information from 167 released wells between 52° and 58°N in the British sector of the North Sea have been studied and measurements of thermal conductivity have been conducted on many samples from all the main stratigraphic units. Although large errors may be associated with the temperature information, it is sufficiently reliable to establish that heat flow is not conserved with depth over much of the western North Sea. In the Central graben and Anglo-Dutch basin, heat flow in the upper 1-2 km (3,300-6,600 ft) is around 50 mW m-2 increasing downward to about 100 mW m-2. …
Regional Geothermal Exploration in North Central New Mexico
The Yermak Plateau: Formed at a triple junction
Terrestrial heat flow in Canada
Heat flow has been measured at 214 separate sites in Canada and on the surrounding continental shelves. Most geological provinces show average heat flow that conforms approximately to world averages for areas of similar tectonic age, but the northern Prairies show an anomalously high heat flow that is probably controlled by deep water movement, and the coastal zone of southern British Columbia shows a low heat flow that is believed to be associated with recent subduction of small ocean plates.
Geothermal measurements in northern British Columbia and southern Yukon Territory
Heat flow and heat production from the Malingsbo granite, central Sweden
Relationships between heat flow, paleotemperatures, coalification and petroleum maturation in the San Juan Basin, northwest New Mexico and southwest Colorado
Across the San Juan Basin both coal rank and heat flow suggest the past and present geothermal influence of a massive thermal source associated with the San Juan volcanic field. Maximum paleotemperature estimates are calculated for the Fruitland Formation coals across the San Juan Basin by correlating coal rank to temperature-maturation charts for the Gulf Coast region, and by considering the effects of paleoclimate, uplift, additional burial and the San Juan volcanic field heat source. Estimated maximum paleotemperatures for the Basin are generally consistent with the regional pretroleum production, oil production occurring in the cooler regions around the western, southern …