References
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The measurement and interpretation of heat flow in the Mediterranean and Black Seas
Heat flow in the Caribbean and Gulf of Mexico
Dannye O Teplovom Rezhime Zemnoi Kory Yugo-zapada BSSR (Data on the Thermal Regime of the Earth's Crust in the Southwest of the BSSR )
Teplovoi Potok V Pripyatskoi Vpadine (Heat Flow in the Pripyat Trough )
The Implications of Terrestrial Heat Flow Observations on Current Tectonic and Geochemical Models of the Crust and Upper Mantle of the Earth
The average heat flow through continental erogenic belts decreases with the age of the orogeny to an approximately constant value for the Precambrian shields and platforms. The average heat flow for provinces of the North Pacific decreases with the age of the province. The mean heat flow through the province younger than 10 million years is 2.82 μ cal cm−2 s−1 whereas the mean heat flow through provinces older than the middle Cretaceous is 1.15 μ cal cm−2s−1. The contrast in the chemical composition of continental and oceanic crustal rocks and the disparity in time scale for the decay of …
The relationship of heat flow, bottom topography and basement relief in peake and freen deeps, Northeast Atlantic
Nine closely spaced heat flow observations were made near 43°N 20°W during a detailed survey of Peake and Freen deeps situated on the eastern side of the Mid-Atlantic Ridge. These values range from 1.23 to 1.76 μcal./cm2·sec and all are close to the Atlantic average of 1.34 μcal./cm2·sec. This result, together with the absence of any known earthquake epicenters, implies that there is no igneous activity in the area at present. The observed scatter in the heat flow values cannot be attributed solely to experimental error but must be partly due to environmental effects. Quantitative estimates of the effects of …
The Barracuda Fault Zone in the western North Atlantic: geological and geophysical studies
Heat Flow Measurements on the Reykjanes Ridge
Terrestrial heat flow in the Celebes and Sulu Seas
Heat flow between the Caribbean Sea and the Mid-Atlantic Ridge
Despite a large variability, a systematic pattern of heat flow is discernable from 41 new measurements between the Caribbean Sea and the mid-Atlantic ridge. The highest values are measured within 200 km of the mid-Atlantic ridge crest, and low heat flow occurs 300 to 600 km west of the ridge crest. A smaller-scale pattern is found from more detailed measurements between fracture zones between 9° and 12°N latitude. The equilibrium heat flux beneath the thickly sedimented floor of the Vema fracture is probably about twice the measured values of 3.0 HFU (?cal/cm2 sec).
Etude sur la distribution des températures en Roumanie
Sea Floor Geothermal Measurements from VEMA Cruise 23
Teplovoj rezhim nedr SSSR (Thermal regime of the USSR interior )
Heat flow in Korea
Twelve new heat flow measurements in South Korea are reported. Excluding one anomalous value, the average heat flow in South Korea was found to be 1.5 · 10−6 cal./cm2·sec which is equal to the world's average. In the area characterized by Tertiary volcanism, high heat flow was observed. The high heat flow region is considered to be a part of the high heat flow region extending from the Japan Sea side of the Japanese islands. The transition from high heat flow to normal or low heat flow occurs rather sharply. It may indicate that the source causing high heat flow …
Detailed geophysical studies on the Hawaiian Arch near 24°25′N, 157°40′W: A closely spaced suite of heat-flow stations
10．北海道における地殻熱流量の測定（その1）
Heat flow studies under upper mantle project
Teplovii Potik Dneprovsko-Donetskoi Za-Padini Ta Donbasu (Heat Flow of the Dnieper-Donetsk Basin (by) Donbass )
Heat-flow measurement in non-homogeneous terrains. Its application to geothermal areas
Taking into account the great importance of thermal prospections in geothermal research, it was decided to give an experimental answer to some questions concerning the measurement in non-homogeneous terrains such as flysch. With this aim, the testing ground was located on flysch having high limestone content in marly clays, in a thermally anomalous area (heat flow = 16.39 · 10−6 cal/cm2 sec). Geological and thermal characteristics of the field, thickness and nature of the whole impervious layer, contact temperature of the latter and the underlying pervious layer were already known, as several deep wells had already been drilled in this …