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地应力作用下鸭绿江断裂带活动对丹东五龙背地热温泉的影响初析

毛佳睿 马秀敏 孙尧 姜景捷 张文汇

毛佳睿,马秀敏,孙尧,等,2023. 地应力作用下鸭绿江断裂带活动对丹东五龙背地热温泉的影响初析[J]. 地质力学学报,29(3):402−416 doi: 10.12090/j.issn.1006-6616.20232909
引用本文: 毛佳睿,马秀敏,孙尧,等,2023. 地应力作用下鸭绿江断裂带活动对丹东五龙背地热温泉的影响初析[J]. 地质力学学报,29(3):402−416 doi: 10.12090/j.issn.1006-6616.20232909
MAO J R,MA X M,SUN Y,et al.,2023. Preliminary analysis of the influence of the activity in the Yalu River fault zone on the Wulongbei geothermal hot springs in Dandong under the action of crustal stress [J]. Journal of Geomechanics,29(3):402−416 doi: 10.12090/j.issn.1006-6616.20232909
Citation: MAO J R,MA X M,SUN Y,et al.,2023. Preliminary analysis of the influence of the activity in the Yalu River fault zone on the Wulongbei geothermal hot springs in Dandong under the action of crustal stress [J]. Journal of Geomechanics,29(3):402−416 doi: 10.12090/j.issn.1006-6616.20232909

地应力作用下鸭绿江断裂带活动对丹东五龙背地热温泉的影响初析

doi: 10.12090/j.issn.1006-6616.20232909
基金项目: 中国地质调查局项目(DD20230249,DD20230014,DD20190546);中国地质科学院地质力学研究所基本科研业务费(DZLXJK202106)
详细信息
    作者简介:

    毛佳睿(1992—),女,博士,助理研究员,主要从事区域地壳稳定性评价、工程地质与地质灾害等研究工作。E-mail:547799801@qq.com

    通讯作者:

    马秀敏(1978—),男,在读博士,教授级高工,主要从事地应力测量及监测、地壳稳定性调查评价等研究工作。 E-mail:maxinmin2@163.com

  • 中图分类号: P315.72+7

Preliminary analysis of the influence of the activity in the Yalu River fault zone on the Wulongbei geothermal hot springs in Dandong under the action of crustal stress

Funds: This research is financially supported by the China Geological Survey Projects (Grants DD20230249, DD20230014 and DD20190546) and the Basic Scientific Research Fund of the Institute of Geomechanics, Chinese Academy of Geological Sciences (Grant DZLXJK202106).
  • 摘要:

    鸭绿江断裂带为郯庐断裂系的重要分支,现今构造活动强烈,沿断裂带出露温泉60余处,地热资源丰富。为查明断裂带南段五龙背地区的现今地应力状态和断层的活动性,研究断裂活动对温泉地热水体的控制作用和远期影响,采用水压致裂法对该区开展了12个测段的原位地应力测量。测量结果显示,在测段深度36.80~215.50 m范围内,最大、最小水平主应力及垂直主应力值(SHShSv)分别为6.00~13.52 MPa、3.18~7.26 MPa和0.97~5.7 MPa,总体而言,3个主应力值呈现随深度的增加而逐渐增大的趋势,最大水平主应力方向以北东向为主;断裂带中段(198.60~207.80 m),主应力关系为SH>Sv>Sh,有利于走滑型活动,具有一定潜力的富水导水条件,断裂带上段(36.80~196.63 m)及下段(215.50 m),SH>Sh>Sv,有利于逆断层活动,热流通道纵向连续性欠佳,导水条件较差;根据现今应力场特征与断裂活动的关系推演,五龙背地区温泉水位下降可能是因为断裂在压应力作用下活动,导水系统空间受挤压逐渐缩小,其他方向径流排泄增多,导致温泉水源供给减少;基于库仑摩擦失稳理论,断裂带36.80~113.20 m深度范围内的地应力值达到了其活动需要的应力临界值下限,将来有可能发生错断活动,温泉地热水体的补给通道可能受到断裂活动的影响而发生改变。研究成果在断裂对温泉地热水体控制作用研究方面具有一定的理论意义,并积极探索了断裂带附近地应力测量在地热研究领域中的应用思路。

     

  • 图  1  研究区地理位置及地质构造简图

    F1—鸭绿江断裂带;F2—蚂蚁岭−五龙背断裂;F3—黄土坎−大堡断裂

    Figure  1.  Geographical location and tectonic diagram of the study area

    F1–Yalu River fault zone; F2–Mayiling–Wulongbei fault; F3–Huangtukan–Dabao fault

    图  2  主要断裂构造与温泉发育关系图(据李文庆,2015修改)

    ①—辽阳弧形断裂;②—寒岭−偏岭断裂带;③—海城−草河口断裂带;④—庄河−桓仁断裂带;⑤—刘家河−青堆子断裂带;⑥—四平街−凤城断裂带;⑦—鸭绿江断裂带;⑧—海城析木城−岫岩断裂带

    Figure  2.  Map showing the relationship between main faults and hot springs (modified from Li, 2015)

    ①–Liaoyang arc-shaped fault; ②–Hanling–Pianling fault zone; ③–Haicheng–Caohekou fault zone; ④–Zhuanghe–Huanren fault zone; ⑤–Liujiahe–Qingduizi fault zone; ⑥–Sipingjie–Fengcheng fault zone; ⑦–Yalu River fault zone; ⑧–Haichengximucheng–Xiuyan fault zone

    图  3  地应力钻孔各测量段水压致裂曲线特征线特征

    Figure  3.  Curves of in-situ stress measured by hydraulic fracturing method in the test borehole

    图  4  地应钻力孔印模定向结果

    Figure  4.  The impression orientation results in the test borehole

    图  5  地应力钻孔主应力大小随深度分布

    Figure  5.  Distribution graph showing the borehole stress with depth

    图  6  丹东五龙背温泉区断裂活动概化图

    F1—鸭绿江断裂带;F2—蚂蚁岭−五龙背断裂;F3—黄土坎−大堡断裂

    Figure  6.  Schematic diagram showing the fault activities in the Wulongbei hot spring area

    F1–Yalu River fault zone;F2–Mayiling–Wulongbei fault;F3–Huangtukan–Dabao fault

    图  7  鸭绿江断裂带及其邻区构造应力场随深度变化

    σ1一最大水平主应力a—上部36.80~196.63 m;b—中部198.60~207.80 m;c—下部215.50 m

    Figure  7.  Diagram showing the tectonic stress field of the Yalu River fault zone with depth

    (a) Upper part (36.80–196.63 m); (b) Middle part (198.60–207.80 m); (c)Lower part (215.50 m)σ1–the maximum horizontal stress

    图  8  鸭绿江断裂带对温泉水位控制作用概念模型

    Figure  8.  Conceptual model of the control effect of the Yalu River fault zone on the water level of the hot springs

    图  9  库仑摩擦滑动准则评价结果和断层应力状态分析

    Figure  9.  Graph displaying evaluation results of Coulomb friction sliding criterion and stress state analysis of the fault

    表  1  鸭绿江断裂带温泉状况

    Table  1.   List of hot springs in the Yalu River fault zone

    温泉名称出露位置采水量/(m3·d−1)水温/℃温泉井数(利用数/总数)
    五龙背 振安区五龙背镇 2300 72 13/19
    炮守营 元宝区炮守营村 700 53 4/4
    东汤 凤城市东汤镇 2400 73 2/2
    草河 凤城市草河经济区 580 40 0/6
    宝山 凤城市宝山镇 120 46 1/1
    北汤 凤城市刘家河镇 / 45 1/2
    汤池子 东港市汤池镇 / 38 1/2
    北井子 东港市北井子镇 240 53 1/1
    椅圈 东港市椅圈镇 200 71 3/3
    合计 / 6990 / 26/39
    下载: 导出CSV

    表  2  地应力钻孔水压致裂地应力测量结果

    Table  2.   Results of the in-situ stress measured by hydraulic fracturing method in the test borehole

    测段深
    度/m
    破裂压力
    Pb/MPa
    重张压力
    Pr/MPa
    瞬时关泵压力
    Ps/MPa
    抗拉强度
    T/MPa
    孔隙水压力
    P0/MPa
    最大水平主应力
    SH/MPa
    最小水平主应力
    Sh/MPa
    垂直主应力
    Sv/MPa
    最大主应
    力方向
    36.807.014.422.822.590.366.003.180.97NE 58.94°
    86.887.395.584.221.810.859.295.072.30
    92.226.735.453.871.280.908.644.772.44
    101.6812.518.086.264.431.0013.527.262.69
    113.207.836.164.911.671.1110.936.023.00
    132.8510.985.613.855.371.309.005.153.52
    144.7012.408.925.493.481.4212.406.913.83
    159.708.745.073.683.671.578.935.254.23NE 80.53°
    196.636.684.883.331.801.938.595.265.20
    198.605.013.662.211.351.956.374.165.25
    207.807.574.632.952.942.047.944.995.50
    215.509.915.784.244.132.1110.596.355.70NE 77.78°
    注:地应力测量孔静水位5.63 m
    下载: 导出CSV
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