阳高—天镇地区高温地热系统形成机制及资源开发前景研究

何亚东, 贾小丰, 张自宾, 宋健, 郭靖, 刘培森, 张森琦, 段江飞. 阳高—天镇地区高温地热系统形成机制及资源开发前景研究[J]. 水文地质工程地质, 2023, 50(4): 39-49. doi: 10.16030/j.cnki.issn.1000-3665.202302065
引用本文: 何亚东, 贾小丰, 张自宾, 宋健, 郭靖, 刘培森, 张森琦, 段江飞. 阳高—天镇地区高温地热系统形成机制及资源开发前景研究[J]. 水文地质工程地质, 2023, 50(4): 39-49. doi: 10.16030/j.cnki.issn.1000-3665.202302065
HE Yadong, JIA Xiaofeng, ZHANG Zibin, SONG Jian, GUO Jing, LIU Peisen, ZHANG Senqi, DUAN Jiangfei. A study of the formation mechanism and resource development prospect of the high-temperature geothermal system in the Yanggao-Tianzhen area[J]. Hydrogeology & Engineering Geology, 2023, 50(4): 39-49. doi: 10.16030/j.cnki.issn.1000-3665.202302065
Citation: HE Yadong, JIA Xiaofeng, ZHANG Zibin, SONG Jian, GUO Jing, LIU Peisen, ZHANG Senqi, DUAN Jiangfei. A study of the formation mechanism and resource development prospect of the high-temperature geothermal system in the Yanggao-Tianzhen area[J]. Hydrogeology & Engineering Geology, 2023, 50(4): 39-49. doi: 10.16030/j.cnki.issn.1000-3665.202302065

阳高—天镇地区高温地热系统形成机制及资源开发前景研究

详细信息
    作者简介: 何亚东(1989-),男,硕士,工程师,主要从事区域地质及地热地质相关研究。E-mail:hyd.310@163.com
    通讯作者: 贾小丰(1982-),男,硕士,高级工程师,主要从事地热(干热岩)资源调查评价及二氧化碳地质储存潜力评价相关研究。E-mail:jiaxiaofeng@mail.cgs.gov.cn
  • 中图分类号: P314

A study of the formation mechanism and resource development prospect of the high-temperature geothermal system in the Yanggao-Tianzhen area

More Information
  • “双碳”背景下,山西省持续深入推进清洁能源发展,2020年3月在大同天镇县水桶寺村附近探获高温高压地热流体。为探究大同阳高—天镇地区高温地热系统及成因机制,选择阳高孤山村—平山村一带20 km2的范围作为重点研究区,采用地质调查、地球物理、钻探、测井等手段查明研究区地热赋存条件和规律。研究结果表明:(1)阳高—天镇地区的地热资源主要赋存于太古界变质岩及断裂带含水岩组中,直接热源可能为中上地壳未冷却的岩浆囊,盖层为第四系堆积物、新近系和古近系砂砾石层。(2)该地区高温地热系统为对流、传导型地热系统:一方面大气降水、地表水经孔隙渗透作用及断层裂隙通道下渗至热储位置受热形成热水,随后沿断裂通道对流上升至浅地表出露成温泉;另一方面新生代以来持续的伸展拉张环境,导致软流圈上涌,上地幔部分熔融形成的基性玄武岩浆经深部断裂通道上升至中上地壳形成多个岩浆囊,热量通过断裂或高热导率值的太古界变质岩传递至浅地表形成地热异常。(3)YG-1井抽水试验结果显示,该地区水热型地热资源以静储量为主,开发利用应考虑采用无干扰换热技术。综合分析区域地质条件,结合物探、钻探成果,认为该地区深部可能存在干热岩型地热资源,有待进一步查证。

  • 加载中
  • 图 1  大同盆地地震分布图(据文献[21-22]修改)

    Figure 1. 

    图 2  二维地震与CSAMT测线布置图

    Figure 2. 

    图 3  云门山断裂带

    Figure 3. 

    图 4  房屋裂缝

    Figure 4. 

    图 5  二维地震反演解释剖面图

    Figure 5. 

    图 6  L3测线二维地震和CSAMT成果解释剖面图

    Figure 6. 

    图 7  CSAMT成果解释剖面图

    Figure 7. 

    图 8  YG-1井钻孔柱状简图

    Figure 8. 

    图 9  YG-1井静稳态测温曲线图

    Figure 9. 

    图 10  阳高地区二维地震反演成果(据文献[6]修改)

    Figure 10. 

    图 11  研究区三维地热系统模型

    Figure 11. 

    表 1  研究区地热井统计表

    Table 1.  Statistics of geothermal wells in the study area

    地热井编号J-1J-2J-3J-8J-4J-46J-58J-45J-18J-19
    用途九龙温泉洗浴云门山温泉洗浴吉祥温泉洗浴阳光 99 温泉洗浴封存封存封存农田灌溉农田灌溉农田灌溉
    孔深/m174195>150>150154178>15096120<100
    孔口温度/℃424545456210490352833
    单位流量/(m³∙h−13050404045504040
    地层时代第四系第四系第四系第四系第四系新太古界第四系第四系第四系第四系
    井口标高/m1 0551 0641 1161 1121 0951 113
    建井时间2 0032 0032 0062 0092 0002 002
    水位埋深/m98.6106.8105.4113.590.3113.4
    年实际开采量/m³36 00028 80028 80028 80000019 20019 200
      注:表中“—”表示数据无法获取。
    下载: 导出CSV
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出版历程
收稿日期:  2023-02-27
修回日期:  2023-04-23
刊出日期:  2023-07-15

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