Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (4): 1236-1246.doi: 10.13278/j.cnki.jjuese.201704204

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Faults and Karsts Controlled Geothermal Genesis Model of Xianrenqiao Hot Spring in Changbai Mountain

Chen Peng, Shan Xuanlong, Hao Guoli, Zhao Rongsheng, Zhou Jian   

  1. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2017-03-02 Online:2017-07-26 Published:2017-07-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41430322,41472304)

Abstract: Xianrenqiao hot spring is a great sparesort of China. We conducted a systematic study to explore the genesis mechanism through the methods of geology, hydrogeology and geophysics, for the purpose of further exploration and sustainable development of geothermal resources. Results show that this area belongs to a low-medium temperature geothermal system of convective type, with a composite geothermal genesis model of faults and karsts. The thermal reservoir was originally Paleozoic Cambrian and Ordovician limestone with poor porosity and permeability, but the reservoir property was greatly improved by the structural and dissolved fractures that formed in later period. The cap rocks are mainly Mesozoic Jurassic andesite and andesitic volcaniclastic rocks with strong sealing capability. The hot spring area origins mainly from the rainfall recharged in the area of Changbai Mountain, seeps into the underground thermal reservoir along the lateral faults and karst fractures; Then the groundwater is gradually heated by the normal heat flow during circulating, forming the geothermal water. The thermal reservoir temperature has been estimated to be 89-118 ℃, with a water circulation depth of 2 853-3 820 m; Finally the geothermal water flows upward in the intersection zones of the NE-and NW-striking faults, forming the Xianrenqiao hot spring. In a word, the area that has intersecting faults and abundant karsts is a favorable and prospective area for the exploration of geothermal water. This conclusion provides a theoretical reference for the exploration of similar geothermal resources.

Key words: Xianrenqiao hot spring in Changbai Mountain, faults, karsts, genesis model, low-medium temperature geothermal system of convective type

CLC Number: 

  • P314
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