References
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Teplovoi Potok Cherez dno Zapadnoi Chernogo Morya (Heat flow through the bottom of the western part of the Black Sea )
Каталог данных по тепловому потоку Сибири (1966-1984 гг.)
Heat flow and lithospheric thinning in the Ligurian Basin (N.W. Mediterranean)
On the thermal structure of the southern Tibetan crust
Heat flow and heat generation in the Churchill Province of the Canadian Shield, and their palaeotectonic significance
Six new heat flow determinations are presented for Proterozoic mobile belts of the Churchill Province of the Canadian Shield, an area that was affected by several stages of the Hudsonian orogenic sequence (1.9-1.6 Ga ago). With other, previously published, values the mean of eight determinations considered reliable and representative and corrected for the effects of Pleistocene glaciation is 44 ± 7 mW m−2. Heat generation measurements have also been made; values range from 0.1–1.04 μW m−3. A linear relation between heat flow and heat production is apparent. The heat flow axis intercept is 37 mW m−2, and the scale depth …
Heat flow study in the Malay basin
Heat flow studies of the circum-Pacific subduction zones
Preliminary report of the marine geophysical and geological surveys off Wilkes Land, Antarctica in 1983-1984
Heat flow in the Balearic and Tyrrhenian basins, western Mediterranean
Thermal structure beneath Tohoku, northeast japan
Combined with geophysical observations and petrological considerations, we have studied the thermal models of the Tohoku (northeast Japan) subduction zone. The temperature of the deeper part of the mantle wedge is constrained by the petrological requirements that demand a high-temperature region (> 1400°C) beneath the volcanic zone. To satisfy this condition, namely to explain the arc volcanism in the Tohoku subduction zone, a high-temperature upper mantle beneath the Japan Sea (possibly 1400°C at the depth shallower than 100 km) is required. Heat flow distribution, which constrains the temperature structure at shallower depth, shows that low heat-flow values ranging from 20 …
A geothermal and geophysical survey on the south flank of the Costa Rica rift: Sites 504 and 505
Heat flow in the Salawati and Bintuni Basins
Heat flow from the West African Shield
Measurement of heat flow on Leg 86 of the Deep Sea Drilling Project
Data Catalog on Heat Flow in Siberia (1966-1984)
A heat-flow reconnaissance southeastern Alaska
Heat flow in Figi
Teplovom Pole V Predelakh Zapadnogo Borta Yuzhno- Kaspiiskoi Depressii - Izvestiya an Turkm Ssr, Ser Fiziko-Tekh- Nicheskikh, Khimicheskikh I Geologicheskikh Nauk (Thermal Field In the Limiting Board of the South Caspian Depression )
Rezul'taty Geotermicheskih Issledovanij V Skv (Geothermal Survey Results in Well )
Heat flow in Eastern Egypt: The thermal signature of a continental breakup
The Red Sea is a modern example of continental fragmentation and incipient ocean formation. Heat flow data have been collected from eastern Egypt to provide information relating to the mode and mechanism of Red Sea opening. Preliminary heat flow data, including new data reported here, are now available from twenty-five sites in eastern Egypt and one site in western Sinai. A pattern of low to normal heat flow (35–55 mW m−2) inland with high heat flow (75–100 mW m−2) in a zone within 30 to 40 km of the coast is indicated. Moderately high heat flow (around 70 mW m−2) …