Genesis and resource assessment of Lindian geothermal field, Heilongjiang Province

MA Yongfa; ZHOU Xuejun; ZHAN Tao; LIU Ling; WANG Xu; DONG Junling; LIU Yu; HE Lan; LIU Yan; LI Chang; SHI Zhenzhen

doi:10.12097/j.issn.1671-2552.2022.12.014

2022 Vol. 41, No. 12

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Article navigation > Geological Bulletin of China > 2022 > 41(12): 2244-2255

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MA Yongfa, ZHOU Xuejun, ZHAN Tao, LIU Ling, WANG Xu, DONG Junling, LIU Yu, HE Lan, LIU Yan, LI Chang, SHI Zhenzhen. Genesis and resource assessment of Lindian geothermal field, Heilongjiang Province[J]. Geological Bulletin of China, 2022, 41(12): 2244-2255. doi: 10.12097/j.issn.1671-2552.2022.12.014

Citation:

MA Yongfa, ZHOU Xuejun, ZHAN Tao, LIU Ling, WANG Xu, DONG Junling, LIU Yu, HE Lan, LIU Yan, LI Chang, SHI Zhenzhen. Genesis and resource assessment of Lindian geothermal field, Heilongjiang Province[J]. Geological Bulletin of China, 2022, 41(12): 2244-2255. doi: 10.12097/j.issn.1671-2552.2022.12.014

Genesis and resource assessment of Lindian geothermal field, Heilongjiang Province

1.
Institute of Ecological Geology Survey and Research of Heilongjiang Province, Harbin 150030, Heilongjiang, China
2.
China University of Geosciences(Wuhan), Wuhan 430074, Hubei, China
3.
Innovation Base of Cold Region Geothermal Energy Application Technology of Northeast China, Geological Society of China, Harbin 150030, Heilongjiang, China

More Information

Corresponding author: ZHOU Xuejun, 13766893593@163.com

Received Date: 29 September 2021

Revised Date: 02 November 2022

Publish Date: 15 December 2022

Abstract

Abstract

In order to establish the genesis model of Lindian geothermal field and accurately evaluate the potential of the geothermal resources, geological exploration including geological survey, geophysical exploration, geothermal drilling, geophysical logging and water level monitoring were employed. The results show that the main heat sources in Lindian geothermal field are mantle-derived heat, radioactive decay heat produced by basement granite and friction heat generated by deep faults. The geothermal reservoir is mainly composed of sandstones. The third and fourth members of the Quantou Formation, the Qingshankou Formation and Yaojia Formation of the Cretaceous are the main reservoirs. The burial depth of the main geothermal reservoir are ca.940 ~ 2062 m, and the accumulated thickness of the reservoir is ca.150 ~ 240 m. Three deep faults, namely Lindian fault, Lindian East fault and Western Boundary Fault of Heiyubao Sag are good channels for conduction of the deep heat to the upper strata. Furthermore, the Nenjiang Formation, the Sifangtai Formation and the Mingshui Formation overlaying the reservoir form a good thermal insulation caprock. According to calculation, the base resources of the Lindian geothermal field reaches 6.95×10¹⁹ J, whereas the volume of the geothermal fluid is 9.78×10¹⁰ m³, and the recoverable geothermal fluid is 9.84×10⁷ m³/a, equaling to a capacity of 694.13 MW, which is equivalent to a large scale geothermal field. According to water level monitoring, withdrawal of the thermal water in Lindian town reached the maximum in 2017, and the water level dropped to the lowest point, which exceeded the maximum allowable withdrawal, thus reinjection is necessary. This research provides technical support for the exploration, exploitation and utilization planning and mining right setting of the Lindian geothermal field in the future.
- genesis model /
- resource assessment /
- Lindian geothermal field /
- Heilongjiang Provine

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