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    多尺度综合地球物理方法在扎西康铅锌锑金多金属矿找矿预测中的应用

    郭镜 李文昌 李光明 焦彦杰 梁生贤

    郭镜, 李文昌, 李光明, 焦彦杰, 梁生贤, 2019. 多尺度综合地球物理方法在扎西康铅锌锑金多金属矿找矿预测中的应用. 地球科学, 44(6): 2129-2142. doi: 10.3799/dqkx.2018.362
    引用本文: 郭镜, 李文昌, 李光明, 焦彦杰, 梁生贤, 2019. 多尺度综合地球物理方法在扎西康铅锌锑金多金属矿找矿预测中的应用. 地球科学, 44(6): 2129-2142. doi: 10.3799/dqkx.2018.362
    Guo Jing, Li Wenchang, Li Guangming, Jiao Yanjie, Liang Shengxian, 2019. Application of Multi-Scale Integrated Geophysical Method in Prospecting Prediction of Zhaxikang Pb-Zn-Sb-Au Polymetallic Deposit. Earth Science, 44(6): 2129-2142. doi: 10.3799/dqkx.2018.362
    Citation: Guo Jing, Li Wenchang, Li Guangming, Jiao Yanjie, Liang Shengxian, 2019. Application of Multi-Scale Integrated Geophysical Method in Prospecting Prediction of Zhaxikang Pb-Zn-Sb-Au Polymetallic Deposit. Earth Science, 44(6): 2129-2142. doi: 10.3799/dqkx.2018.362

    多尺度综合地球物理方法在扎西康铅锌锑金多金属矿找矿预测中的应用

    doi: 10.3799/dqkx.2018.362
    基金项目: 

    国家自然科学基金青年科学基金项目 41604118

    国家重点研发计划深地资源开采项目 2016YFC0600308

    中国地质调查局地质调查项目 DD20160015

    详细信息
      作者简介:

      郭镜(1985-), 工程师, 勘探地球物理专业

      通讯作者:

      李文昌(1962-), 教授, 博士生导师

    • 中图分类号: P611

    Application of Multi-Scale Integrated Geophysical Method in Prospecting Prediction of Zhaxikang Pb-Zn-Sb-Au Polymetallic Deposit

    • 摘要: 青藏高原后碰撞阶段发生了大规模地壳尺度的伸展作用, 并在特提斯喜马拉雅带内发育了淡色花岗岩、南北及东西向断裂等构造-热事件, 形成了一系列的铅锌锑金多金属矿床.扎西康铅锌锑金多金属矿是带内已发现唯一的超大型多金属矿床.应用多尺度的综合地球物理方法开展扎西康矿区的找矿预测, 为特提斯喜马拉雅铅锌锑金成矿带内的矿床勘查提供借鉴.首先, 通过穿越错那洞穹窿、藏南拆离系(STDS)及扎西康典型矿床的南北向MT剖面(长72 km, 基准点距1 km), 初步建立了扎西康矿床深部构造-热事件的空间关系, 结合区域构造-热事件的时间关系, 提出了构造-热耦合成矿作用模型, 为扎西康的地球物理勘探提供基础.其次, 通过1:5万区域重力(线距500 m, 点距400 m)和MT剖面(点距500 m)浅部信息的联合解译, 对扎西康整装勘查区尺度的导矿构造开展研究.最终, 通过激电中梯扫面测量(线距100 m, 点距40 m)、AMT剖面(点距50 m)及重力剖面(点距20 m)的联合解译, 对扎西康的含矿断裂开展研究, 定位深部隐伏矿体.

       

    • 图  1  特提斯喜马拉雅后碰撞阶段构造-热事件时空分布

      a.特提斯喜马拉雅地质矿产简图,反映了主要的构造-热事件(图据张进江等,2011修改;数据源自郑有业等, 2007, 2014孟祥金等,2008张建芳,2010);b.特提斯喜马拉雅后碰撞阶段构造-热事件时间序列示意图(数据源自Searle et al., 1997Yin et al., 1999Blisniuk et al., 2001Lee and Whitehouse, 2007Aikman et al., 2008Williams et al., 2001Liu et al., 2014

      Fig.  1.  Temporal and spatial distribution of tectonic-thermal events in the Tethys Himalayan post-collision phase

      图  2  (a) MT剖面反演图;(b)MT剖面解译的构造-热事件空间分布图;(c)重力剖面反演解译图

      Fig.  2.  (a) Inversion of MT section; (b) Tectonic-thermal event spatial distribution map from MT profile interpretation; (c) Inversion and interpretation map of gravity profile

      图  3  后碰撞伸展期特提斯喜马拉雅铅锌锑金成矿带构造-热事件成矿作用示意

      Fig.  3.  Schematic diagram of Tethys Himalaya Pb-Zn-Sb-Au metallogenic belt tectonic-thermal event coupling metallogenic model in post-collisional extension stage

      图  4  (a) 扎西康矿集区地质简图;(b)铅锌矿体典型剖面

      Zhou et al.(2017)修改

      Fig.  4.  (a) Geology map of Zhaxikang deposit, (b) Pb-Zn sectional view of body

      图  5  扎西康整装勘查区岩石密度统计结果

      Fig.  5.  Statistical results of rock density in Zhaxikang area

      图  6  (a) 扎西康整装勘查区1:5万高精度重力测量密度三维反演解译图;(b)MT剖面浅部信息反演解译图

      Fig.  6.  (a) 3-D inversion interpretation diagram of 1:50 000 high-precision gravity measurement in Zhaxikang integrated ex- ploration area; (b) shallow information inversion interpretation diagram of MT section

      图  7  扎西康ZK4006钻孔岩心电阻率与极化率变化曲线

      Fig.  7.  Resistivity and polarizability curve of ZK4006 drill in Zhaxikang

      图  8  (a) 激电中梯面积测量视极化率图;(b)激电中梯面积测量视电阻率图;(c)AMT反演解译图;(d)重力剖面反演解译图

      Fig.  8.  (a) Polarizability map of IP measurement, (b) resistivity map of IP measurement, (c) inversion and interpretation map of AMT, (d) inversion and interpretation map of gravity profile

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