References
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Determination of heat flow values in the two granitic rock regions of Japan - Houfu area in Yamaguchi Prefecture and Kunisaki area in Oita Prefecture, Southwest Japan
Heat flow, structure and evolution of the lithosphere of Mongolia
A heat flow profile across the Sverdrup Basin, Canadian Arctic Islands
Geothermal measurements in the northern Red Sea: Implications for lithospheric thermal structure and mode of extension during continental rifting
Report on DELP 1987 Cruises in the Ogasawara Area : Part VI: Heat Flow Measurements
Novye dannye o teplovom potoke Zapadnoj Sibiri (New data on the heat flow in Western Siberia )
Geotermichecky razrez Pechenegskoy structur (Geothermal section of the Pechenga structure )
Scientific Cruise Report of Arctic Expedition ARK IV/3
Teplovoj potok vpadiny Chernogo morja (Heat flow in the Black Sea basin )
New heat flow investigations in Arkansas
Heat flow in the Witwatersrand Basin and environs, and its significance for the South African shield geotherm and lithospheric thickness
Heat Flow and Tectonics of the Ligurian Sea Basin and Margin
A review of temperature, thermal conductivity, and heat flow data from the Pannonian Basin
More than 2700 pieces of data have been selected from evaluation of all available temperature measurements made in boreholes in Hungary. They comprise steady-state temperatures, drill stem test data, and corrected outflowing water temperatures. These data have been used to construct average temperature versus depth profiles for different subu-nits of the central part of the Pannonian basin in Hungary.
Heat-flow and water-chemistry data from the Cascade Range and adjacent areas in north-central Oregon
Thermal Regime of the State 2–14 Well, Salton Sea Scientific Drilling Project
Temperature logs were made repeatedly during breaks in drilling and both during and after flow tests in the Salton Sea Scientific Drilling Project well (State 2–14). The purpose of these logs was to assist in identifying zones of fluid loss or grain and to characterize reservoir temperatures. At the conclusion of the active phase of the project, a series of logs was begun in an attempt to establish the equilibrium temperature profile. Initially, we were able to log to depths below 3 km, but beginning in late May of 1986, it was impossible to log below about 1.8 km owing …
Tunisian geothermal data from oil wells
Since direct measurements of steady-state temperatures are not readily available in Tunisia, a geothermal investigation has been made using 1319 values of bottom-hole temperatures (BHTs) obtained from 217 petroleum exploration wells. An empirical relation based on the differences between BHT and DST (drill stem tests) was used to correct BHTs and estimate geothermal gradients.The estimated geothermal gradient of the country varies between 21 and 52 degrees C/km. A few regions with similar gradients have been identified, and similarities between gradient contours and the main structural directions are noted. Furthermore, for 25 points from 12 wells, it was possible to apply …