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青海省共和县恰卜恰干热岩体地热地质特征

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文章导航 > 中国地质 > 2018 > 45(6): 1087-1102

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张森琦, 严维德, 黎敦朋, 贾小丰, 张盛生, 李胜涛, 付雷, 吴海东, 曾昭发, 李志伟, 穆建强, 程正璞, 胡丽莎. 2018. 青海省共和县恰卜恰干热岩体地热地质特征[J]. 中国地质, 45(6): 1087-1102. doi: 10.12029/gc20180601
引用本文: 张森琦, 严维德, 黎敦朋, 贾小丰, 张盛生, 李胜涛, 付雷, 吴海东, 曾昭发, 李志伟, 穆建强, 程正璞, 胡丽莎. 2018. 青海省共和县恰卜恰干热岩体地热地质特征[J]. 中国地质, 45(6): 1087-1102. doi: 10.12029/gc20180601
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ZHANG Senqi, YAN Weide, LI Dunpeng, JIA Xiaofeng, ZHANG Shengsheng, LI Shengtao, FU Lei, WU Haidong, ZENG Zhaofa, LI Zhiwei, MU Jianqiang, CHENG Zhengpu, HU Lisha. 2018. Characteristics of geothermal geology of the Qiabuqia HDR in Gonghe Basin, Qinghai Province[J]. Geology in China, 45(6): 1087-1102. doi: 10.12029/gc20180601
Citation: ZHANG Senqi, YAN Weide, LI Dunpeng, JIA Xiaofeng, ZHANG Shengsheng, LI Shengtao, FU Lei, WU Haidong, ZENG Zhaofa, LI Zhiwei, MU Jianqiang, CHENG Zhengpu, HU Lisha. 2018. Characteristics of geothermal geology of the Qiabuqia HDR in Gonghe Basin, Qinghai Province[J]. Geology in China, 45(6): 1087-1102. doi: 10.12029/gc20180601
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青海省共和县恰卜恰干热岩体地热地质特征

  • 1.

    中国地质调查局水文地质环境地质调查中心, 河北 保定 071051

  • 2.

    青海省国土资源厅, 青海 西宁 810001

  • 3.

    福州大学紫金矿业学院, 福建 福州 350116

  • 4.

    青海省水文地质工程地质环境地质调查院, 青海 西宁 810008

  • 5.

    吉林大学地球探测科学与技术学院, 吉林 长春 130026

  • 6.

    中国科学院测量与地球物理研究所大地测量与地球动力学国家重点实验室, 湖北 武汉 430077

  • 7.

    中国冶金地质总局地球物理勘查院, 河北 保定 071051

  • 基金项目:
    中国地质调查局地质调查项目（DD20160192、DD20179033、DD20179621）资助
详细信息
    作者简介: 张森琦, 男, 1962年生, 硕士, 教授级高级工程师, 主要从事地热地质与水工环地质调查研究工作; E-mail:senqizhang@126.com
    通讯作者: 付雷, 男, 1986年生, 硕士, 工程师, 主要从事地热地质与水工环地质调查研究工作; E-mail:pengyou0808@163.com

  • 中图分类号: P314.2

Characteristics of geothermal geology of the Qiabuqia HDR in Gonghe Basin, Qinghai Province

  • 1.

    Center for Hydrogeology and Environmental Geology Survey, China Geological Survey, Baoding 071051, Hebei, China

  • 2.

    Department of Land and Resources of Qinghai, Xining 810002, Qinghai, China

  • 3.

    School of Zijin Mine, Fuzhou University, Fuzhou 350116, Fujian, China

  • 4.

    Institute of Hydrogeology, Engineering Geology and Environmental Geology Survey of Qinghai, Xining 810008, Qinghai, China

  • 5.

    School of Resources and Environment, Jilin University, Changchun 130026, Jilin, China

  • 6.

    State Key Lab of Geodesy and Geodynamics, Chinese Academy of Sciences, Wuhan 350116, Hubei, China

  • 7.

    Geophysical Exploration Institute of China Metallurgical Geology Bureau, Baoding 071000, Hebei, China

  • Fund Project: Supported by China Geological Survey Program (No. DD20160192, DD20179033, DD20179621)
More Information
    Author Bio: ZHANG Senqi, male, born in 1962, master, professor, mainly engages in the study of geothermal geology, hydrogeology, and environmental geology survey and research; E-mail: senqizhang@126.com .
    Corresponding author: FU Lei, male, born in 1986, master, engineer, majors in the study of geothermal geology, hydrogeology, and environmental geology survey and research; E-mail:pengyou0808@163.com

    摘要

  • 基于地热地质、综合地球物理勘查成果等布孔依据，实施的GR1干热岩勘探孔位于共和县恰卜恰干热岩体中南部，是迄今我国钻遇地层温度最高的干热岩勘探孔，为我国首个EGS示范工程与科研试验平台建设奠定了基础。GR1孔测温结果表明，2500 m深处温度为150℃，进入干热岩段；终孔深度3705 m处的井底温度为236℃。2500~3705 m井段平均地温梯度为71.4℃/km，高于另3眼干热岩勘探孔；2800~3705 m井段地温梯度大于80℃/km，属中等品质以上干热岩。综合地球物理勘查与4眼干热岩勘探孔钻探结果表明，该干热岩体埋深2104.31~2500 m，面积246.90 km2；干热岩资源评价结果表明，3~5 km深度范围，100年内的潜在发电装机容量为3805.74 MW，以2%的采收率计，装机容量为76.11 MW；3~6 km潜在装机容量为7788.26 MW，以2%的采收率计，装机容量为155.77MW；3~7 km潜在装机容量为13639.25 MW，以2%的采收率计，装机容量为272.79 MW。

    Based on regional geology, geothermal geology and integrated geophysical exploration results, the GR1 hot dry rock exploration well was completed in the central part of Qiabuqia Town in the Gonghe basin. The GR1 well is the highest temperature hot-dry rock exploration well in China, which has laid an important foundation for China's first EGS demonstration project. The temperature measurement results show that the temperature at the depth of 2500 m is 150℃, entering into the hot dry rock section. The temperature of the bottom hole at the depth of 3705 m is 236℃. The average geothermal gradient of 2500-3705 m is 71.4℃/km, which is higher than that of the other 3 hot dry rock exploration wells. At 2800-3705 m of GR1 well the geothermal gradient is higher than 80℃/km. The exploration results show that the depth of the hot dry rock is 2104.31-2500 m, which is oval-shaped in the east-west direction, with an area of 246.90 km2. The evaluation results show that the total theoretical resources of the Qiabuqia hot dry rock is 1638.16EJ in the depth of 3-5 km, equivalent to 55.909 billion tons of standard coal.

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  • 图 1  研究区大地构造位置图(张雪亭等，2007)

    Figure 1. 

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    图 2  共和地区区域地层(a)与GR1孔实钻地层结构图(b)

    Figure 2. 

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    图 3  共和盆地周边印支期以来主要花岗岩体分布图

    Figure 3. 

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    图 4  共和县上塔买村—克才村—东坡村温泉分布图

    Figure 4. 

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    图 5  基于高精度航磁数据推断的恰卜恰干热岩体范围图

    Figure 5. 

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    图 6  过恰卜恰镇南北向AB剖面重磁人机交互反演结果图

    Figure 6. 

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    图 7  共和地区21 km以上深度水平S波速度结构图

    Figure 7. 

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    图 8  恰卜恰地区干热岩勘探孔分布图

    Figure 8. 

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    图 9  GR1干热岩勘探孔井深-温度曲线图

    Figure 9. 

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    图 10  GR1孔干热岩段岩心柱状图

    Figure 10. 

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    图 11  基于钻孔资料推断的恰卜恰干热岩体分布图

    Figure 11. 

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    图 12  东西向大地电磁测深（MT）勘查提供的热源信息

    Figure 12. 

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    表 1  共和盆地周缘造山带印支期主要岩体统计

    Table 1.  Statistical table of rock masses of orogenic belt surrounding Gonghe Basin in the Indosinian periods

    下载: 导出CSV

    表 2  恰卜恰地区地热与干热岩钻孔统计

    Table 2.  Geothermal and hot dry rock drilling statistics in Qiabuqia area

    下载: 导出CSV

    表 3  GR1孔随钻留点温度计测温结果

    Table 3.  The temperature measurement results during drilling with thermometer in GR1 well

    下载: 导出CSV

    表 4  恰卜恰地区干热岩勘探孔统计

    Table 4.  The statistical table of HDR exploration wells in Qiabuqia area

    下载: 导出CSV

    表 5  中国干热岩资源调查评价阶段初步划分方案

    Table 5.  Preliminary divisions of investigation and evaluation stage for China's dry hot rock resources

    下载: 导出CSV
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收稿日期:  2018-03-28
修回日期:  2018-06-10
刊出日期:  2018-12-25

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