References
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Heat flow and conduction-dominated thermal regimes
Zakladny vyskum priestoroveho rozlozenia zemskeho tepla v zapadnych karpatoch (in Slovak)
Heat flow in Italy
Novye Geotermi- Cheskie Issedovaniya Na Ozere Baikal - V Kn: Seismichnost I Glubin- Noe Stroenie Pribaikalia Novosibirsk: Nauka, (Geothermal research in Baikal using a cable thermometer probe )
Novye geotermal'nye issledovanija na ozere Bajkal (New geothermal research on the lake Baikal )
Heat flow measurement in the Port More borehole
Conductive heat flows in research drill holes in thermal areas of Yellowstone National Park, Wyoming
Heat flow through the Dead Sea rift
Heat flow and heat production studies in north dakota
Terrestrial heat flow and crustal radioactivity in northeastern New Mexico and southeastern Colorado
Measurement and interpretation of terrestrial heat flow in Israel
Sixty-eight new determinations of terrestrial heat flow in Israel have a range of 0.17-11.07 μcal/cm2s. The average value of deep conductive heat flow in the undisturbed complex of the Arabo-Nubian Massif is 0·94 μcal/cm2s; it is least affected by circulation of groundwater. This value is only slightly higher than the heat flow of 0·88 μcal/cm2s in the Levantine Basin of the Mediterranean Sea. Several values that exceed 2·0 μcal/cm2s are due either to (probable) deep hydrothermal activity or to small domal structures of the basement. Within the sedimentary sequence which blankets the crystalline massif, terrestrial heat flow is often redistributed …
Hydrocarbon Habitat of Tertiary Niger Delta1
The Tertiary Niger delta covers an area of about 75,000 sq km and is composed of an overall regressive clastic sequence which reaches a maximum thickness of 30,000 to 40,000 ft (9,000 to 12,000 m). The development of the delta has been dependent on the balance between the rate of sedimentation and the rate of subsidence. This balance and the resulting sedimentary patterns appear to have been influenced by the structural configuration and tectonics of the basement.Structural analysis of the Tertiary overburden shows that individual fault blocks can be grouped into macrostructural and eventually megastructural units. Such megaunits are separate …
Review of heat flow data from the eastern Mediterranean region
Nouvelles determinations du flux geothermique en France (New determinations of geothermal flow in France)
Geotermicheskie osobennosti Ural'skoj geosinklinal (Geothermal features of the Ural geosyncline )
Geophysical surveys for Leg 59 sites, Deep Sea Drilling Project
Heat flow measurements in Yellowstone Lake and the thermal structure of the Yellowstone Caldera
Twenty-two marine-type heat flow determinations in Yellowstone Lake indicate a rapid transition from high heat flow values outside the Yellowstone caldera, 100?300 mW m?2 (2.5?7.5 ?cal cm?2 s?1), to an extensive area of very high heat flow, 600?700 mW m?2 (14.5 ?cal cm?2 s?1) and greater, within the caldera. The thermal transition occurs 5?10 km inside the mapped caldera boundary and approximately coincides with the point at which a zone of earthquake activity beginning outside the caldera terminates. Higher heat flow in West Thumb and Mary Bay (about 1600 mW m?2 (40 ?cal cm?2 s?1)) outlines two thermal subprovinces within …