贵州息烽温泉控热推覆构造的发现及成因研究

张蕊1, 2, 牟雨亮1, 2, 朱立军1, 王甘露1, 2, 曾波3. 2023. 贵州息烽温泉控热推覆构造的发现及成因研究. 中国地质调查, 10(1): 45-51. doi: 10.19388/j.zgdzdc.2023.01.05
引用本文: 张蕊1, 2, 牟雨亮1, 2, 朱立军1, 王甘露1, 2, 曾波3. 2023. 贵州息烽温泉控热推覆构造的发现及成因研究. 中国地质调查, 10(1): 45-51. doi: 10.19388/j.zgdzdc.2023.01.05
ZHANG Rui, MOU Yuliang, ZHU Lijun, WANG Ganlu, ZENG Bo, . 2023. Discovery of geothermal nappe structure and genesis research of Xifeng hot spring in Guizhou. Geological Survey of China, 10(1): 45-51. doi: 10.19388/j.zgdzdc.2023.01.05
Citation: ZHANG Rui, MOU Yuliang, ZHU Lijun, WANG Ganlu, ZENG Bo, . 2023. Discovery of geothermal nappe structure and genesis research of Xifeng hot spring in Guizhou. Geological Survey of China, 10(1): 45-51. doi: 10.19388/j.zgdzdc.2023.01.05

贵州息烽温泉控热推覆构造的发现及成因研究

  • 基金项目:

    贵州省自然资源厅"贵州省地质勘查基金项目(编号: 2017-02)"资助

详细信息
    作者简介: 张蕊(1998—),女,硕士研究生,主要从事非常规油气、地热地质工作。Email: 695039887@qq.com
  • 中图分类号: P314.1

Discovery of geothermal nappe structure and genesis research of Xifeng hot spring in Guizhou

  • 根据近年来磷矿深部勘探资料,对贵州息烽温泉的构造地质条件及地热特征开展研究,获得了有关温泉地质成因的新认识。①由洋水背斜、安清断层(F1)和温泉断层(F2)组成的叠瓦状逆冲推覆构造体系,构成了息烽温泉地热水系统的主体及边界,该控热构造体系内地表构造与地腹构造并不统一,老地层盖在新地层上,构成顶、底两层叠置的多个热储单元,这些热储单元是地热水形成和运移的良好场所。②安清断层(F1)使多个热储单元直接接触,从而具有密切的水力联系,为导水、导热的良好通道; 温泉断层(F2)构成了息烽温泉区地热水系统的边界。③大气降水沿断裂通道下渗至深部的碳酸盐岩热储层中,吸收热量形成地热水,在高温高压条件下,向洋水背斜核部进行迁移,受上覆寒武系碎屑岩盖层的保护和温泉断层的限制,形成洋水背斜西翼和北端的地热资源有利富集区,最后受分支断层阻挡而自然岀露。
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出版历程
收稿日期:  2021-07-23
修回日期:  2021-11-02
刊出日期:  2023-02-20

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