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References

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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
1987

Heat flow off Sumatra

Lawrence A. Lawver, Patrick T. Taylor
No preview available
Acta Seismologica Sinica, 1987

Geothermal Observation in East Liaoning and Haicheng Seismic area

Andong Wang, Yuhe Ren, Wenfu Sun, Longwei Yu, Jingming Liang, Tianqing Cao, Haoding Gu

We have obtained altogether heat flux data of 23 drill holes including 2 observational holes of thermal flow in the Haicheng seismic area. These data show roughly thermal structure of crust in east Liaoning and the Haicheng seismic area. The results indicate that there is higher rate of heat flow in the north by east belt from Liaoyang to,Xiongyue, and the average thermal flux is 8.2910-2 J/m2s (2.0 HFU). Average thermal flux in the Haicheng seismic area is 9.2210-2J/m2s (2.2 HFU).Comparing with other known geophysical data of the Haicheng seismic area, we give a geophysical section of synthetic interpretation. We …

1987

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

A. H. Lachenbruch, B. V. Marshall, E. F. Roth
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Geothermics, 1987

Heat flow and heat generation estimates for the Churchill basement of the western Canadian Basin in Alberta, Canada

R.D.W. Beach, F.W. Jones, Jacek A. Majorowicz

Heat flow through the sediments and temperatures of the Churchill province basement under the sedimentary cover are determined for 24 locations in the central part of the Prairies basin in Alberta where the vertical heat flux is approximately constant from the base of the sediments to the surface. The contribution to heat flow from heat generation in the sediments is also considered. The average heat flow through the sediments is found to be 71 mWm−2 ± 12 mWm−2 which is about 30mWm−2 higher than in the neighbouring shield area of the Churchill province, and the contribution from heat generation in …

1987

A study of waste-heat recovery and utilization at the Raton Public Service Company Municipal Power Plant: Final technical report

Roy A Cunniff
No preview available
Chinese Science Bulletin, 1987

Heat flow measurements in Panzhihua-Xichang (Panxi) paleorift zone, SW China

Jiyang Wang, Jian Wang, Shao-Peng Huang, Wen-Ren Zhang, Yousong Zhou, Xin Jun
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1987

Final report geothermal resource assessment, South Dakota

William D. Gosnold Jr
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Doklady Akademii Nauk SSSR (Reports of the USSR Academy of Sciences), 1987

Anomalii teplovogo potoka v moskovskoi i baltiiskoi sineklizakh (Heat flow anomalies in the Moscow and Baltic syneclines )

Vadim V. Gordienko, Olga V. Zavgorodnyaya
No preview available
Geophysical Research Letters, 1987

Heat flow at the proposed Appalachian ultradeep core hole (ADCOH) site: Tectonic implications

John K. Costain, Edward R. Decker
No preview available
1987

Data report of hydrographic observation

Hydrographic Department of Maritime Safety Agency
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 …

Geothermal Resources Council Transactions, 1987

Geothermal data from deep holes in the Oregon Cascade Range

David D. Blackwell, John L. Steele
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Methods in Experimental Physics, 1987

14. Experimental Methods in Continental Heat Flow

David D. Blackwell, Robert E. Spafford

Publisher Summary Heat flow measurements are made for a number of purposes and the techniques vary depending on the intended use. Because the internal processes of the earth are thermally driven, heat flow measurements are typically used to study tectonics. Regional heat flow values contain information on the thermal structure of the lithosphere and some aspects of the geochemistry of the crust. This chapter discusses the equipment for measurement of temperature, thermal conductivity, and heat production from radioactive decay. It describes the equipment associated with well testing and reservoir evaluation and/or determination of various water flow parameters. These methods are …

1987

Investigations of the UK Heat Flow Field (1984-1987): Investigation of the Geothermal Potential of the UK

J.S. Gebski, J. Wheildon, A.A. Thomas-Betts
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1987

Mesure du flux de chaleur à Ririwai, delta du Niger (Nigéria)

C. Chukwueke
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Exploration Geophysics, 1987

Thermal conductivity and heat flow in the southern Cooper Basin

Kerry Gallagher
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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 …

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

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
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