References
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Heat flow, heat production and granite depth in western France
Newly measured heat flow and full heat production determinations over the Armorican Massif, Western France, are tested against a linear relationship as proposed through Birch's law. The data do not fit a strict linear relationship but are within an elongated cluster which can be approximated (in mW/m² and km) by: These parameters are compared with those of surrounding Hercynian regions. Data from the Central Massif and previously failed to fit any linear relationship. Data for Scotland and Southern England could not be fitted to a single line. However, the present data and those from Southern and Central England do fit …
Problematyka hydro geotermiczna regionu sudeckiego
Heat flow measurements on the Bay of Plenty coast, New Zealand
Deep sea drilling project geothermal measurements: A review
Heat Flow Values of the 5th Ggt in China
Geothermal energy in Tunisia: Potential of the southern province
The aim of this paper is to obtain a first reliable evaluation of the geothermal potential of Tunisia. Thanks to various existing geological, hydrogeological and petroleum data, it was possible to distinguish the main geothermal features of the country, by evaluating both the underground temperature and the potential reservoirs. Hot springs, either the already known or newly inventoried, have been analysed and a few geothermometers applied: SiO2, Na/K and Na-K-Ca. Only the SiO2 gave plausible values with 90°C as a maximum temperature. A detailed geothermal study was also focused on the greatest sedimentary basin of the country (Southern Tunisia), where, …
Linear relationship between heat flow and heat production in Panxi Paleorift Zone, southwestern China
Heat flow density measurements in northern Morocco
Two sets of data are used to estimate heat flow density in Morocco: 36 determinations were made in shallow boreholes (100–500 m) in equilibrium conditions and 44 determinations in oil exploration boreholes (1000–5000 m). These two sets of data are apparently consistent and are used to define the gross feature of heat flow in northern Morocco: Anti-Atlas, located at the West African craton boundary, is affected by a low heat flow (40 ± 5 m Wm−2) close to the average value obtained in this craton (37 ±8 m Wm−2); Mesetas, formed by a paleozoic and mesozoic basement, are characterized by …
Heat flow and tectonics of the northwestern Pacific subduction zones -concerning the Yap Trench convergence
Geothermal heat flux at the COST B-2 and B-3 Wells, US Atlantic continental margin
Risulti delle Misure di Flusso di Calore nel Mare di Sardegna
Zhangzhou basin geothermal system - genesis model, energy potential and the occurrence of thermal water
Zhang zhou basin geothermal system is the highest in temperature in the southeastern "geothermal zone" (excluding Taiwan). Up to present, the highest temperature measured is 106℃ at the well head and 121.5 ℃ at the bottom of the drillhole, respectively. Artesian wells in the center of the geothermal field may reach the largest flowrate of more than 500 tons per day. The thermal water production of a single well may surpass 15,00 tons per day(10m. depression in the groundwater table). The common chemical type of thermal water is Cl-Na type. The highest T. D. S. is 12 gram per liter, …