References
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Heat flow: heat production studies in Nova Scotia
Results of some geothermal studies in Singhbhum Thrust Belt, India
Bericht über Temperaturmessungen bei Landau/Pfalz
Heat flow measurements in Northern Italy and heat flow maps of Europe
Heat flow at arrival heights, Ross Island, Antarctica
Heat flow measurements in the Norwegian Sea
Cold spot in west Africa—Anchoring the African Plate
Teplovoi Potok V Armenii (Heat flow in Armenia )
Basic heat-flow data from the United States
Heat flow from eastern Panama and northwestern Colombia
Heat flows were determined at 12 sites in four distinct areas between longitude 77° and 80°W in eastern Panama and northwestern Colombia. Evidently, most of the region is underlain by mafic oceanic crust so that the crustal radiogenic component of heat flow is very small (∼ 0.1 μcal cm−2 sec−1). Low heat-flow values (∼ 0.7 μcal cm−2 sec−1) in northwestern Colombia may reflect thermal transients associated with shallow subduction. The normal values (∼ 1) at about 78°W are consistent with the mean heat flow from the western Caribbean and the Gulf of Mexico. At 80°W, a fairly high value of …
Novye dannye o teplovom potoke cherez dno v Ohotskom more (New data on heat flow through the bottom in the Sea of Okhotsk)
Heat flow northeast of Guadeloupe Island, Lesser Antilles
Five new heat flow measurements combined with previously published data in the area of the Barracuda ridge indicate relatively low values (average 0.97 HFU) associated with the ridge. The fractured nature of the Barracuda ridge and the distribution of the heat flow values suggest that the low values are the result of mass water flow, which may have reduced the heat flow, normally assumed to be due to conduction.
Geothermal measurements on Leg 22 of the D/V Glomar Challenger
The Galapagos Spreading Centre: Heat-flow low on the North Flank
The axis of the Galapagos spreading centre has a high but variable heat flow. A distinct local minimum in the heat-flow field exists in a region 4–6 My old on the northern flank of the spreading centre. This minimum is unlikely to have been produced from refraction of heat flux due to either topographic and sediment thickness irregularities or to the transient effect of sediment loading. We suggest that the oceanic crust has an ‘effective’ permeability to fluid flow and that hydrothermal circulation causes much of the heat loss to arise through mass transport. This mechanism also lowers the conductive …
Geotermicheskiye issledovaniya v Zapadnoy Sibiri (Geothermal research in Western Siberia )
Thermal Regime of Deep Temperate Dimictic Lakes
Glubinnyj Teplovoj potok v Severnoj i Central'nojChastjah Vostochno-Evropejskoj platformy (Deep Heat Flow in the North and Central Parts of the East European Platform)
Teplovoj potok, gidrotermal'naja aktivnost' i dinamika razvitija glubinnyh zon oblastej kajnozojskogo vulkanizma (Heat flow, hydrothermal activity and development dynamics of the deep zones of Cenozoic volcanism )
Heat flow, radioactive heat generation, and theoretical tectonics for northwestern Mexico
Nine heat flow values from Baja California and Sonora represent the first determinations of heat flux from Mexico and, in general, justify southerly extensions of the Basin and Range and Southern California thermal provinces of the southwestern United States. Heat flow in northern Baja California is low (0.84 hfu), consistent with known values from the Sierra Nevada Batholith, but a value of 1.23 hfu was recorded in the central area of the peninsula. Seven measurements from Sonora, averaging 2.5 hfu, are similar to Basin and Range values. Reduced heat flow values (q*) have been calculated for Sonora and are interpreted …
Heat-flow — heat-generation studies in Norway
Fifteen heat-flow determinations based on data from 34 drill holes throughout central and southern Norway are presented. Five combined heat-flow — heat-generation measurements from homogeneous Precambrian and Permian crystalline rocks from southern Norway confirm a linear relation between heat flow and heat generation of the form Q = Q0 + bA, where Q is surface heat flow (1hfu = 10−6 cal cm−2 sec−1), A is surface heat generation (1hgu = 10−13 cal cm−3 sec−1), and b and Q0 are constants. The slope of the line (b = 8.4 km) is in good agreement with results obtained from other stable continental …