沧县隆起中部大地热流及岩石圈热结构特征：以献县地热田为例

段和肖; 刘彦广; 王贵玲; 边凯; 牛小军; 牛飞; 胡静

doi:10.3799/dqkx.2022.070

Volume 48 Issue 3

Mar. 2023

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Article Navigation > Earth Science > 2023 > 48(3): 988-1001

Duan Hexiao, Liu Yanguang, Wang Guiling, Bian Kai, Niu Xiaojun, Niu Fei, Hu Jing, 2023. Characteristics of the Terrestrial Heat Flow and Lithospheric Thermal Structure in Central Cangxian Uplift: A Case Study of Xianxian Geothermal Field. Earth Science, 48(3): 988-1001. doi: 10.3799/dqkx.2022.070

Citation:

Duan Hexiao, Liu Yanguang, Wang Guiling, Bian Kai, Niu Xiaojun, Niu Fei, Hu Jing, 2023. Characteristics of the Terrestrial Heat Flow and Lithospheric Thermal Structure in Central Cangxian Uplift: A Case Study of Xianxian Geothermal Field. Earth Science, 48(3): 988-1001. doi: 10.3799/dqkx.2022.070

Citation:

Duan Hexiao, Liu Yanguang, Wang Guiling, Bian Kai, Niu Xiaojun, Niu Fei, Hu Jing, 2023. Characteristics of the Terrestrial Heat Flow and Lithospheric Thermal Structure in Central Cangxian Uplift: A Case Study of Xianxian Geothermal Field. Earth Science, 48(3): 988-1001. doi: 10.3799/dqkx.2022.070

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Characteristics of the Terrestrial Heat Flow and Lithospheric Thermal Structure in Central Cangxian Uplift: A Case Study of Xianxian Geothermal Field

doi: 10.3799/dqkx.2022.070

Duan Hexiao^{1, 3
,
,},
Liu Yanguang^{1, 2, 3
,
,},
Wang Guiling^{2, 3},
Bian Kai³,
Niu Xiaojun⁴,
Niu Fei⁴,
Hu Jing⁵

1.
School of Earth Sciences and Engineering, Hebei University of Engineering, Handan 056000, China
2.
Technology Innovation Center for Geothermal & Hot Dry Rock Exploration and Development, Ministry of Natural Resources, Shijiazhuang 050061, China
3.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China
4.
Hydrogeological Team, Hebei Coalfield Geology Bureau, Handan 056000, China
5.
School of Civil Engineering and Architecture, Jiangsu University of Science and Technology, Zhenjiang 212100, China

Received Date: 2022-02-25
Available Online: 2023-03-27
Publish Date: 2023-03-25

Abstract

Abstract

Understanding the lithospheric thermal structure is an important basis for understanding the continental dynamics (i.e., tectonic deformation and evolution) of the continental lithosphere. It is also the core of studies on the thermal source mechanisms of geothermal fields. Most importantly, it can provide scientific guidance for the exploration and development of deep geothermal resources. The Cangxian uplift enjoys rich geothermal resources and favorable geothermal geological conditions. However, its lithospheric thermal structure is still unclear, which restricts the exploration and development of regional geothermal resources. Focusing on the Xianxian geothermal field in the middle part of the Cangxian uplift through the temperature measurement of a 4 000 m deep well and fine tests of geotechnical thermophysical properties, this study has ascertained the characteristics of the terrestrial heat flow and lithospheric thermal structure in the study area, thus filling the gap in terrestrial heat flow measurement. Moreover, this study has established a conceptual model of the lithospheric thermal structure of the study area and estimated the deep temperature and lithospheric thickness in the study area. The results show that the Xianxian geothermal field has a heat flow of 70.58 mW/m², a burial depth of the Curie surface of about 24 km, a Moho temperature of about 749 ℃, and a lithospheric thickness of about 85-96 km.
- Cangxian uplift,
- Xianxian geothermal field,
- terrestrial heat flow,
- lithospheric thermal structure,
- geothermal energy

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References(59)

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Characteristics of the Terrestrial Heat Flow and Lithospheric Thermal Structure in Central Cangxian Uplift: A Case Study of Xianxian Geothermal Field

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