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References

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Geophysical Research Letters, 1987

Heat flow, heat production and granite depth in western France

J.L. Vigneresse, Jean Jolivet, M. Cuney, Gerard Bienfait

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 …

Prozeglad Geologiczny (Geological Review), 1987

Problematyka hydro geotermiczna regionu sudeckiego

Jan Dowgiallo
No preview available
Journal of Volcanology and Geothermal Research, 1987

Heat flow measurements on the Bay of Plenty coast, New Zealand

B. Simpson
No preview available
Reviews of Geophysics, 1987

Deep sea drilling project geothermal measurements: A review

Roy D. Hyndman, Marcus G. Langseth Jr, Richard P. Von Herzen
No preview available
1987

Heat Flow Values of the 5th Ggt in China

Shuxing Liang, etal.
No preview available
Geothermics, 1987

Geothermal energy in Tunisia: Potential of the southern province

Hamed Ben Dhia

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, …

Geophysical Research Letters, 1987

Linear relationship between heat flow and heat production in Panxi Paleorift Zone, southwestern China

Ji-Yang Wang, Shao-Peng Huang
No preview available
Journal of African Earth Sciences, 1987

Heat flow density measurements in northern Morocco

Abdelkrim Rimi, Francis Lucazeau

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 …

1987

Heat flow and tectonics of the northwestern Pacific subduction zones -concerning the Yap Trench convergence

Seiichi Nagihara
No preview available
1987

Geothermal heat flux at the COST B-2 and B-3 Wells, US Atlantic continental margin

Bruno Della Vedova, Richard P. Von Herzen
No preview available
Annual meeting of the National Group of Geophysics of the Solid Earth, 1987

Risulti delle Misure di Flusso di Calore nel Mare di Sardegna

Bruno Della Vedova, Giulio Pellis
No preview available
1987

Zhangzhou basin geothermal system - genesis model, energy potential and the occurrence of thermal water

Zhonghe Pang

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, …

1987

Mapas geotermais do Brasil

Valiya M. Hamza, A. Frangipani, E.A. Becker
No preview available
Tikhookeanskaya geologiya (Pacific geology), 1987

Novye dannye o geotermike Tatarskogo proliva (New data on geothermics of the Tatar Strait )

Yuri V. Shevaldin, Valery I. Balabashin, Petr S. Zimin
No preview available
Revista Brasileira de Geofisica, 1987

Geothermal gradients inside water wells of east Oweinat area, south western desert of Egypt

Fouad K. Boulos
No preview available
1987

Two-dimensional finite element models of the variation of heat flow with depth caused by refraction at a low conductivity graben

R. W. Saltus, A. H. Lachenbruch
No preview available
1987

Thermal measurements in Oak Springs Formation at the Nevada Test Site, southern Nevada

A. H. Lachenbruch, B. V. Marshall, E. F. Roth
No preview available
Geophysical Research Letters, 1987

Heat flow and basement radioactivity in Maine: First‐order results and preliminary interpretations

Edward R. Decker
No preview available
Tectonophysics, 1987

Geothermal studies in the Hyderabad granitic region and the crustal thermal structure of the Southern Indian Shield

Mohan L. Gupta, S.R. Sharma, A. Sundar, S.B. Singh
No preview available
Izdatelstvo nedra (Subsoil publishing house), 1987

Geotermiya neftegazonosnykh oblastey zapadnoy sibiri - moscow (Geothermy of oil and gas bearing regions of western siberia )

A.R. Kurchikov, B.P. Stavitsky
No preview available