References

Teplovoj potok v Ukrainskom shhite v svjazi s nedavnimi tektonicheskimi dvizhenijami (Heat flow in the Ukrainian Shield in relation to recent tectonic movements )

New heat-flow measurements in the Caribbean and western Atlantic

Terrestrial heat flow near Washington, D.C

Subsurface temperatures and heat flow in the AMSOC core hole near Mayaguez, Puerto Rico

Terrestrial flow of heat in the Brent Crater

Differentsialnaya termometriya neftyanykh i gazovykh skvazhin (Differential thermometry of oil and gas wells )

Evidence for connection between heat flow and the mid-atlantic ridge magnetic anomaly

Fourteen crossings of the crest of the mid-Atlantic ridge between 30° and 6°S revealed the presence of a continuous magnetic intensity anomaly characteristic of the crest of the ridge. Nearly all values of geothermal heat flow greater than 2.0 ?cal/cm2 sec lie within 100 km of the apex of the magnetic anomaly. The continuity of the ridge is interrupted probably by east-west strike-slip faults. Where this occurs, it is likely that the heat-flow pattern is displaced along with the crest.

Heat flow measurements during the JEDS-6 and JEDS-7 cruises in 1963

Geothermal measurements in the twin shaft of Hosszuheteny

Terrestrial heat flow in the Carpathians

Untersuchungen über den Wärmestrom der Erde in Westdeutschland

Terrestrial heat flow in Japan

Heat-flow measurements between North America and the Hawaiian Islands

From 23 new measurements, the average terrestrial heat flow through the deep-sea floor between North America and Hawaii is about 1.4 · 10−6 cal./cm2 sec. No significant differences were measured between recognized topographic provinces, which include the Hawaiian ridge and the Molokai fracture zone.

Some measurements of heat flow through the floor of the north Atlantic

Teplovoi Potok Iz Zem-Nykh Nedr V Raione Krivogo Roga (Heat Flow from the Earth's Subsoil in the Krivoy Rog Area )

Osnovy OpredeleniyaTeplovogo Potoka Iz Zemnykh Nedr I Rezultaty Izmerenii (Fundamentals of Determining Heat Flow from the Earth's Interior and Measurement Results )

Heat flow values from eastern Australia

Heat flows have been measured at seven sites in eastern Australia. The values confirm high heat flow in eastern Australia?about 2.0 ?cal/cm2 sec. The values are in the range 2.0 to 2.9 ?cal/cm2 sec, with the exception of values of 1.0 and 1.2 from two oil wells on the eastern edge of the Great Artesian Basin. The full significance of the latter values can only be assessed as part of a comprehensive geothermal survey of the Basin.

Heat-flow values from the precambrian shield of western Australia

The geothermal flux has been determined for three points on the Western Australian Precambrian shield from temperature measurements in depressed drilled holes and laboratory determinations of thermal conductivity of core samples from the holes. The values (in ?cal/cm2 sec) are: for Kalgoorlie 0.96, for Coolgardie, 0.90, and for Norseman 1.01, with a precision of better than 10 per cent. The temperature measurements show that, in semiarid areas, the intermittent presence of water in a salt lake bed has an appreciable effect on temperatures measured in drilled holes in the immediate vicinity of the lake. Although surface geology varies among the …

Vostochno-Predkavkazskii Artezianskii Bassein (East Pre-Caucasus Artesian Basin )

Geothermal gradients and heat flow in the Salt Valley anticline, Utah

Temperatures- were measured 5 welles located on or near the Salt Valley anticline, Utah. Geothermal gradients in the' section of Mancos Shale (Cretaceous) to Morrison Formation (Jurassic) in the graben area of the anticline ranged from 0.02Qj3oF to 0.0216()oF per foot, or 37.4oC to 39.4oC per km.In . the Hermosa Formation (Pennsylvanian) in the southern area of the anticline, the geothermal gradient is 0.01621