广东惠州花岗岩体及其地热意义

旷健; 祁士华; 王帅; 肖志才; 张敏; 赵旭; 甘浩男

doi:10.3799/dqkx.2019.128

Volume 45 Issue 4

Apr. 2020

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Article Navigation > Earth Science > 2020 > 45(4): 1466-1480

Kuang Jian, Qi Shihua, Wang Shuai, Xiao Zhicai, Zhang Min, Zhao Xu, Gan Haonan, 2020. Granite Intrusion in Huizhou, Guangdong Province and Its Geothermal Implications. Earth Science, 45(4): 1466-1480. doi: 10.3799/dqkx.2019.128

Citation:

Kuang Jian, Qi Shihua, Wang Shuai, Xiao Zhicai, Zhang Min, Zhao Xu, Gan Haonan, 2020. Granite Intrusion in Huizhou, Guangdong Province and Its Geothermal Implications. Earth Science, 45(4): 1466-1480. doi: 10.3799/dqkx.2019.128

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Granite Intrusion in Huizhou, Guangdong Province and Its Geothermal Implications

doi: 10.3799/dqkx.2019.128

Kuang Jian^{1
,
,},
Qi Shihua^{1, 2
,
,
,},
Wang Shuai²,
Xiao Zhicai¹,
Zhang Min³,
Zhao Xu⁴,
Gan Haonan⁵

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
3.
Team 935 of Guangdong Nonferrous Metals Geological Bureau, Huizhou 516001, China
4.
Petroleum Engineering and Geophysics Co., Ltd., SINOPEC, Wuhan 430223, China
5.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China

Received Date: 2019-05-29
Publish Date: 2020-04-15

Abstract

Abstract

In this paper, it presents a case study of the high-temperature geothermal field in Huizhou, China to interpret the formation model of this geothermal field and that of Southeast China by integrating seismics, geochemistry and the zircon U-Pb age. It is found that the magmatic intrusion in the study area is mainly Yanshanian I-type granite with high differentiation and high heat-producing elements, which has been formed by the subduction and the retreat of Paleo-Pacific Plate. The subterranean magmatic intrusion is an integrated whole with thickness up to 3.5 km. The heat transfer from the mantle to the surface promoted by the high thermal conductivity of granite, and the heat generated by radioactive element decay in granite are two important causes for high temperature geothermal formation in Huizhou. The subterranean granite in the study area has high heat production and inestimable geothermal resources of hot dry rock. The geothermal output model of this study area is of great significance to the energy supply system in Huizhou and even the Southeast China.
- geothermic,
- seismic inversion,
- Yanshanian granite,
- Paleo-Pacific Plate,
- heat production,
- Southeast China,
- geothermal fields

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References(50)

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Granite Intrusion in Huizhou, Guangdong Province and Its Geothermal Implications

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