山西忻州盆地地热水地球化学特征及其成因机制

张梦昭; 郭清海; 刘明亮; 刘强

doi:10.3799/dqkx.2022.087

Volume 48 Issue 3

Mar. 2023

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Zhang Mengzhao, Guo Qinghai, Liu Mingliang, Liu Qiang, 2023. Geochemical Characteristics and Formation Mechanisms of the Geothermal Waters in the Xinzhou Basin, Shanxi Province. Earth Science, 48(3): 973-987. doi: 10.3799/dqkx.2022.087

Citation:

Zhang Mengzhao, Guo Qinghai, Liu Mingliang, Liu Qiang, 2023. Geochemical Characteristics and Formation Mechanisms of the Geothermal Waters in the Xinzhou Basin, Shanxi Province. Earth Science, 48(3): 973-987. doi: 10.3799/dqkx.2022.087

Citation:

Zhang Mengzhao, Guo Qinghai, Liu Mingliang, Liu Qiang, 2023. Geochemical Characteristics and Formation Mechanisms of the Geothermal Waters in the Xinzhou Basin, Shanxi Province. Earth Science, 48(3): 973-987. doi: 10.3799/dqkx.2022.087

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Geochemical Characteristics and Formation Mechanisms of the Geothermal Waters in the Xinzhou Basin, Shanxi Province

doi: 10.3799/dqkx.2022.087

Zhang Mengzhao^{1, 2
,
,},
Guo Qinghai^{1, 2
,
,
,},
Liu Mingliang³,
Liu Qiang⁴

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
2.
School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
3.
College of Resources and Environment, Yangtze University, Wuhan 430100, China
4.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2021-07-19
Available Online: 2023-03-27
Publish Date: 2023-03-25

Abstract

Abstract

Studies on geothermal water geochemistry are of great significance for understanding the genesis of various hydrothermal resources. By taking the Xinzhou basin in Shanxi Province as a study area, this paper aims to identify the geochemical origin of the Xinzhou geothermal waters, to evaluate the mixing process between the geothermal waters and the shallow cold groundwaters, and to reveal the geological genesis of the Xinzhou geothermal system based on a systematic geochemical study conducted there. The formation of the Xinzhou geothermal system should have nothing to do with a shallow magma chamber or excessive decay heat of radioactive elements in shallow rocks. Instead, it occurred as a result of the deep groundwater circulation in a normal heat flow background. The atmospheric precipitation in the western Yunzhongshan recharge area infiltrated into the deep underground and migrated to the Xinzhou basin with circulation depths between 1 618.3 and 3 451.5 m. Correspondingly, the reservoir temperatures ranged from 48.4 to 91.8 ℃. The geothermal waters were mixed substantially with the shallow groundwaters when ascending to the Quaternary aquifers, the highest mixing ratio being up to 78 %.
- geothermal water,
- geochemistry,
- reservoir temperature,
- heat source,
- Xinzhou basin

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References(58)

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Geochemical Characteristics and Formation Mechanisms of the Geothermal Waters in the Xinzhou Basin, Shanxi Province

doi: 10.3799/dqkx.2022.087

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