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| 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 |
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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.
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Received: 16 September 2005
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2006, Vol. 15 
