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《Geotectonica Et Metallogenia》 1992-03
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TERRESTRIAL HEAT FLOW AND ITS TECTONIC SIGNIFICANCE IN YUNNAN, CHINA

XU Qnig (Central-South University o.f Technology, Changsha, 410083)WANG Jian WANG Jichang ZHANG Wenren (Institute of Geology, Academia Sinica)  
In this paper, 29 reliable heat flow data in Yunnan area, China, are obtained, based on a number of borehole geotemperature logging, thermal conductivity determination on rock-sample, The terrain correction on heat flow values has been conducted where topography is rugged. According to geological characteristics and heat flow values, the area can be divided into the following subareas: 1)Tengchong diwa region, west of Nujiang River, with high heat flow (93.6 mW/m~2 in average); 2) Western Yunnan diwa subarea, with moderate heat flow (59.2mW/m~2 in average); 3) Kunming region of Sichuan-Yunnan diwa system, Southernmost part of North-South diwa area, with high heat flow 85.4 mW/m~2 in average; 4) diwa region around Lijiang-Eryuan with average heat flow 80mW/m~2, 5) the subarea of Southeast Yunnan with low heat flow ranging from 37 to 70mW/m~2, half of which are smaller than 50mW/m~2. In summary, the heat flow values are relatively high and heat flow data are variable, which corresponds to the geological characteristics of the study area.
【Fund】: 国家自然科学基金项目《滇西地区古特提斯构造演化》地热
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