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青藏高原如角高温地热系统构造-热耦合成热模式

郭镜, 唐发伟, 官辉, 赵海华, 赵小云, 旦增国杰, 杜炳锐. 2023. 青藏高原如角高温地热系统构造-热耦合成热模式[J]. 中国地质, 50(6): 1621-1631. doi: 10.12029/gc20220323004
引用本文: 郭镜, 唐发伟, 官辉, 赵海华, 赵小云, 旦增国杰, 杜炳锐. 2023. 青藏高原如角高温地热系统构造-热耦合成热模式[J]. 中国地质, 50(6): 1621-1631. doi: 10.12029/gc20220323004
GUO Jing, TANG Fawei, GUAN Hui, ZHAO Haihua, ZHAO Xiaoyun, DANZENG Guojie, DU Bingrui. 2023. Structure-thermal coupling model of the high temperature geothermal system in Rujiao on the Xizang Plateau[J]. Geology in China, 50(6): 1621-1631. doi: 10.12029/gc20220323004
Citation: GUO Jing, TANG Fawei, GUAN Hui, ZHAO Haihua, ZHAO Xiaoyun, DANZENG Guojie, DU Bingrui. 2023. Structure-thermal coupling model of the high temperature geothermal system in Rujiao on the Xizang Plateau[J]. Geology in China, 50(6): 1621-1631. doi: 10.12029/gc20220323004

青藏高原如角高温地热系统构造-热耦合成热模式

  • 基金项目:
    四川省科技计划项目应用基础研究面上项目(2019YJ0269)、中国地质调查局项目(DD20190033)、西藏自然资源厅项目(54000021210200001054)联合资助
详细信息
    作者简介: 郭镜,男,1985年生, 硕士,高级工程师,从事金属矿产及地热地球物理勘查工作;E-mail: 313756811@qq.com
    通讯作者: 唐发伟,男,1979年生,高级工程师,从事矿产地球化学勘查工作;E-mail: 37205958@qq.com
  • 中图分类号: P314

Structure-thermal coupling model of the high temperature geothermal system in Rujiao on the Xizang Plateau

  • Fund Project: Supported by the applied basic research project of Sichuan Science and Technology Program (No.2019YJ0269); the project of China Geological Survey (No.DD20190033) and the project of Xizang Natural Resources Department (No.54000021210200001054)
More Information
    Author Bio: GUO Jing, male, born in 1985, master, senior engineer, engaged in geophysical exploration of metallic minerals and geothermal; E-mail: 313756811@qq.com .
    Corresponding author: TANG Fawei, male, born in 1979, senior engineer, engaged in geochemical exploration of mineral resources; E-mail: 37205958@qq.com
  • 研究目的

    地表热异常的形成无外乎两方面原因:异常的热源及异常的热传递方式。“厚壳”与“热壳”共存,是青藏高原高温地热系统与一般汇聚板缘型地热系统的最大差异。部分熔融(热)作为“热壳”中的异常热源,断裂系统(构造)作为“厚壳”中的对流传热通道,清晰刻画两者空间关系,探讨构造-热耦合成热模式,可能是完善“厚壳”与“热壳”共存下青藏高原特色成热理论的重要途径。

    研究方法

    本次研究以萨嘎县如角沸泉为例,运用大地电磁测深、音频大地电磁测深。

    研究结果

    探测断裂系统与部分熔融的空间关系;结合已有地球物理、地热地球化学研究,建立如角沸泉构造-热耦合成热模式;并以断裂系统的交汇处为目标体,布设两口生产井。

    结论

    如角式构造-热耦合成热模式具有普适性,对于完善青藏高原特色成热理论及提高地热勘查成功率具有重要意义。

  • 加载中
  • 图 1  青藏高原大地构造及高温热泉分布简图(底图据张进江等,2007)

    Figure 1. 

    图 2  西藏萨嘎县如角沸泉地质简图(据西藏地热队,2021

    Figure 2. 

    图 3  多尺度大地电磁探测如角地热系统流体运移通道

    Figure 3. 

    图 4  如角高温地热系统构造-热耦合成热模式

    Figure 4. 

    图 5  如角地热系统流体动力学分析

    Figure 5. 

    图 6  穿过扎西康温泉的南北向大地电磁测深剖面(据Guo et al., 2019修改)

    Figure 6. 

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出版历程
收稿日期:  2022-03-23
修回日期:  2022-08-19
刊出日期:  2023-12-25

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