References
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Thermal regime of the northern Bay of Biscay continental margin in the vicinity of DSDP sites 400 to 402
Regional variations in Australian heat flow
Geothermal Characteristics of the Rio Grande Rift within the Southern Rocky Mountain Complex
Summary Regionally averaged heat flows along the Rio Grande rift and within the San Juan volcanic field (2.56 ± 0.65 HFU and 2.85 ± 0.65 HFU–excluding values greater than 4.0 HFU) suggest partial melting at depths of 15 to 55 km. Analysis of the half-width of the anomaly along the Rio Grande rift also suggests a thermal source at 20 to 30 km. The somewhat higher averaged heat flow in the San Juan volcanic field may indicate a shallower, or larger volume, or hotter partial melting. Regionally averaged heat flow along the transition zone from the eastern ranges of the …
Geothermal characteristics of the colorado plateau
New heat-flow measurements in the Colorado Plateau varying in depth from 400 to 1900 m suggest that the heat flux throughout the region is 1.5 HFU and greater (1 HFU = 41.8 mW/m2). Along the eastern and southern boundaries of the Plateau, near the San Juan volcanic field and the Mogollon Slope respectively, high heat flows (̆2.2 HFU) are observed to intrude 50–100 km into the Plateau. It is believed that the high heat flows are associated with the sources of the volcanics in those areas. In the interior areas of the Plateau, away from the major volcanic phenomena along …
Termicheskaya Razvedka Mestorozhdenii V UsloviyakhStrukturno-Geologicheskikh Neodnorodnostei (Thermal Exploration of Deposits in Conditions of Structural and Geological Inhomogeneities )
Heat Flow and the Hydrologic Cycle: Examples from Israel
The surface pattern of terrestrial heat flow in Israel is a product of several coexisting mechanisms. Within the sedimentary sequence blanketing over the Precambrian basement of the Arabo-Nubian Massif deep terrestrial heat flow is redistributed, particularly within the depth range of the active hydrologic cycle, by ground water movement. A dense fault network, associated mostly with the Jordan-Dead Sea-Red Sea Rift, facilitates the hydro-logic recharge and discharge system, generating occurrence of numerous hot springs. In the recharge regions, where cool meteoric waters percolate into the subsurface, heat flow values as low as 7.1 mWm−2 were observed. In discharge regions, with …
Heat flow in Moomba, Big Lake and Toolachee gas fields of the Cooper Basin and implications for hydrocarbon maturation
Terrestrial heat flow in Washington county, southeast Ohio
Heat flow and the geothermal potential of Egypt
Preliminary heat flow values ranging from 42 to 175 mW m−2 have been estimated for Egypt from numerous geothermal gradient determinations with a reasonably good geographical distribution, and a limited number of thermal conductivity determinations. For northern Egypt and the Gulf of Suez, gradients were calculated from oil well bottom hole temperature data; east of the Nile, and at three sites west of the Nile, gradients were calculated from detailed temperature logs in shallow boreholes. With one exception, the heat flow west of the Nile and in northern Egypt is estimated to be low, 40–45 mW m−2, typical of a …
Hot springs and geothermal gradients in northern Thailand
Cyprus heat flow with comments on the thermal regime of the eastern Mediterranean
Teplovoj potok na severo-zapade Tihogo okeana Priroda (Heat flow in the Pacific Northwest )
Geothermics of Hungary and the tectonophysics of the Pannonian Basin "red spot"
Heat flow in CSR (Tepelny tok v csr)
Geotermicheskie Issledovaniya - V Kn: Geologo-Geofizi- Cheskie I Podvodnye Issledovaniya Ozera Baikal Moskva: Institut Okea- Nologii an Sssr, (Geothermal Research)
Heat flow measurements under some lakes in the Superior Province of the Canadian Shield
Thermal structure under the ground in Osaka plain, southwest Japan
Heat Flow in South Korea
The hydrothermal mounds of the Galapagos Rift: Observations with DSRV Alvin and detailed heat flow studies
Ranging in height from gentle hills of less than a meter to steep-sided giants of more than 20 m, the mounds of the Galapagos Rift are spectacular hydrothermal features. Their internal temperatures have been measured at up to 13°C above the bottom water temperature, and total heat flow (conducted plus convected) can be several hundred to several thousand times the normal oceanic values. Fluids, when they discharge from the mound, do so at a very slow rate and at temperatures probably quite near the bottom water temperature. The mounds are principally composed of iron silicates intermixed and incrusted with lesser …