北京南口—孙河断裂带水热系统特征与成因分析

雷晓东, 胡圣标, 杨全合, 姜光政, 李娟, 李晨, 张超, 高堋. 2017. 北京南口—孙河断裂带水热系统特征与成因分析. 地球物理学报, 60(5): 1838-1850, doi: 10.6038/cjg20170519
引用本文: 雷晓东, 胡圣标, 杨全合, 姜光政, 李娟, 李晨, 张超, 高堋. 2017. 北京南口—孙河断裂带水热系统特征与成因分析. 地球物理学报, 60(5): 1838-1850, doi: 10.6038/cjg20170519
LEI Xiao-Dong, HU Sheng-Biao, YANG Quan-He, JIANG Guang-Zheng, LI Juan, LI Chen, ZHANG Chao, GAO Peng. 2017. Characteristics of hydrothermal system and its origin of Nankou-Sunhe fault in Beijing. Chinese Journal of Geophysics (in Chinese), 60(5): 1838-1850, doi: 10.6038/cjg20170519
Citation: LEI Xiao-Dong, HU Sheng-Biao, YANG Quan-He, JIANG Guang-Zheng, LI Juan, LI Chen, ZHANG Chao, GAO Peng. 2017. Characteristics of hydrothermal system and its origin of Nankou-Sunhe fault in Beijing. Chinese Journal of Geophysics (in Chinese), 60(5): 1838-1850, doi: 10.6038/cjg20170519

北京南口—孙河断裂带水热系统特征与成因分析

  • 基金项目:

    中国地质调查局项目(12120114033901),昌平新城地热资源调查评价项目(TC1408CBF),京津冀协同发展区主要活动断裂地球物理探测项目(121201104000150012)联合资助

详细信息
    作者简介:

    雷晓东,男,1983年生,博士研究生,高级工程师,主要从事地热资源地球物理勘探技术方面的研究. E-mail:lei-xiaodong@139.com

  • 中图分类号: P314

Characteristics of hydrothermal system and its origin of Nankou-Sunhe fault in Beijing

  • 中低温对流型地热资源在华北地区广泛分布,是一种清洁的替代能源.与活动断裂带相关的水热型地热资源是中低温地热系统的重要组成部分.本文基于高精度重力测量、微动测深及钻孔温度测量等数据,从热源、通道、储层和盖层四个方面探讨了南口—孙河断裂带水热系统特征.低重力异常揭示的燕山期花岗二长岩、闪长岩岩体范围为23.8 km2和14.3 km2,放射性测井数据计算得到其生热率均值为3.14 μW·m-3,侏罗系火山岩生热率均值为1.65 μW·m-3,隐伏岩体和火山岩均难以构成地热系统的附加热源.重力异常显示南口—孙河断裂带宽度约500~800 m,断裂带切割蓟县系雾迷山组白云岩热储层.钻井温度曲线显示断裂带内水热活动强烈,说明该断裂带是导水、导热的重要通道.断裂带南西侧马池口一带第四系松散层与侏罗系火山岩形成了热储盖层,微动测深显示火山岩最大厚度约1500 m.综上源、通、储、盖四个要素分析,该地热系统为热传导—对流复合型,来自京西北山区的大气降水经远距离径流深循环吸收地层热量后沿南口—孙河断裂上移到达裂隙发育的白云岩地层中形成热水.总之,沿南口—孙河断裂带具备了良好的地热地质条件,可达到规模开采的条件.

  • 加载中
  • 图 1 

    研究区基岩地质构造及工作布置图

    Figure 1. 

    Locations of work stations and tectonic background of survey area

    图 2 

    布格重力异常 (a) 与剩余重力异常等值线图 (b)

    Figure 2. 

    Maps of Bouguer anomalies (a) and residual gravity anomalies (b)

    图 3 

    不同方向布格重力异常水平梯度图

    Figure 3. 

    Horizontal-gradient map of Bouguer gravity anomaly in different direction

    图 4 

    AA′和BB′剖面二维微动视S波速度剖面图

    Figure 4. 

    2D microtremor apparent S-wave velocity section of profile along AA′ and BB′

    图 5 

    ZK2孔温度-深度分布及其地温梯度图

    Figure 5. 

    Temperature logs and gradient for borehole ZK2

    图 6 

    水热系统成因模式图

    Figure 6. 

    Accumulation model of hydrothermal system

    表 1 

    测温钻孔信息表

    Table 1. 

    Temperature information of boreholes

    井号 东经/E 北纬/N 测温段/m 井底温度/℃ 地温梯度(℃·km-1) 测温地层
    ZK1 116°07′11.69″ 40°12′25.88″ 0~783.2
    783.2~2204.8
    33.0
    48.5
    27.2
    10.9
    Q
    Jxw
    ZK2 116°09′34.03″ 40°13′09.18″ 0~800.0
    800.0~1052.0
    33.2
    35.4
    27.5
    6.3
    Q
    J+Jxw
    ZK3 116°10′15.03″ 40°13′23.99″ 0~1503.7 32.8 13.8 Q+Jxw
    ZK4 116°10′56.88″ 40°13′39.18″ 0~3315.0 49.7 12.0 Q+Jxw+Jxy+Chg
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出版历程
收稿日期:  2016-10-19
修回日期:  2017-03-14
上线日期:  2017-05-05

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