STUDY ON THE ENRICHING REGULARITY OF GEOTHERMAL WATER IN THE MESO-CENOZOIC BASINS IN LIAONING PROVINCE
NI Jin1, FENG Li-jie1, YAN Bao-qiang1, TIAN Lin-hao2,3
1. Liaoning Institute of Geology and Mineral Resources Survey, Shenyang 110032, China; 2. Inner Mongolia Institute of Geological Survey, Hohhot 010020, China; 3. Institute of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China
Abstract：Rich geothermal resources are hosted in the Meso-Cenozoic basins in Liaoning Province. The geothermal fields are broadly distributed, with stable thermal reservoir horizons and high geotemperature. The water-rich host rocks contain large geothermal energy resources, with a great exploration potential. The geothermal in the deep of the basins can be divided into four sections, i.e. 1) the shallow buried reservoir at the basement upwarping; 2) the deeply buried reservoir at the block raising; 3) the ultra-deep reservoir at the center of basin; and 4) the transitional section of low-middle temperature disturbed by cold water.
倪金, 冯丽杰, 闫宝强, 田林浩. 辽宁省中新生代盆地地下热水富集规律研究[J]. 地质与资源, 2006, 15(1): 57-61,19.
NI Jin, FENG Li-jie, YAN Bao-qiang, TIAN Lin-hao. STUDY ON THE ENRICHING REGULARITY OF GEOTHERMAL WATER IN THE MESO-CENOZOIC BASINS IN LIAONING PROVINCE. GEOLOGY AND RESOURCES, 2006, 15(1): 57-61,19.
2006, Vol. 15 
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