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《Chinese Journal of Geophysics》 2006-01
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Features of heat flow and the geothermal field of the Qinshui Basin

SUN Zhan-Xue, ZHANG Wen, HU Bao-Qun, PAN Tian-YouDepartment of Civil Engineering and Environmental Engineering, East China Institute of Technology, Jiangxi Fuzhou 344000, China  
Based on temperature logging data of 20 boreholes and thermal conductivities of 39 rock samples, 20 heat flow values are calculated for the Qinshui Basin, Shanxi Province, China. The results show that the heat flow values range from 44.8 mW/m~2 to 101.8mW/m~2, with the average 62.7±15.2 mW/m~2, and that the present geothermal gradient varies from 20.9 ℃/km to 47.6 ℃/km with the mean value of 28.2±10.3 ℃/km in the basin. Similarities of the distribution of heat flow to that of coal-bed methane-bearing capacity of the upper and the lower coal beds in the area suggest that the present geothermal conditions reflect the characteristics of the fossil geothermal background during the formation period of coal-bed methane in the basin to some extent.
【Fund】: 国家重点基础研究发展规划项目(2002CB211704)资助.
【CateGory Index】: P314
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