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基于多源遥感数据的纳米比亚欢乐谷地区千岁兰断裂带识别及新发现

王俊虎 武鼎 张杰林 郭帮杰

王俊虎, 武鼎, 张杰林, 郭帮杰. 基于多源遥感数据的纳米比亚欢乐谷地区千岁兰断裂带识别及新发现[J]. 地质科技通报, 2020, 39(5): 183-190. doi: 10.19509/j.cnki.dzkq.2020.0630
引用本文: 王俊虎, 武鼎, 张杰林, 郭帮杰. 基于多源遥感数据的纳米比亚欢乐谷地区千岁兰断裂带识别及新发现[J]. 地质科技通报, 2020, 39(5): 183-190. doi: 10.19509/j.cnki.dzkq.2020.0630
Wang Junhu, Wu Ding, Zhang Jielin, Guo Bangjie. Identification and new discovery of Qiansxuilan fault belt in Gaudeanmus area, Namibia based on the multi-source remote sensing data[J]. Bulletin of Geological Science and Technology, 2020, 39(5): 183-190. doi: 10.19509/j.cnki.dzkq.2020.0630
Citation: Wang Junhu, Wu Ding, Zhang Jielin, Guo Bangjie. Identification and new discovery of Qiansxuilan fault belt in Gaudeanmus area, Namibia based on the multi-source remote sensing data[J]. Bulletin of Geological Science and Technology, 2020, 39(5): 183-190. doi: 10.19509/j.cnki.dzkq.2020.0630

基于多源遥感数据的纳米比亚欢乐谷地区千岁兰断裂带识别及新发现

doi: 10.19509/j.cnki.dzkq.2020.0630
基金项目: 

国家预先研究项目 遥Y1902

详细信息
    作者简介:

    王俊虎(1982-), 男, 高级工程师, 主要从事遥感与GIS在铀成矿环境分析及远景预测方面的研究工作。E-mail:tcwjh2013@126.com

  • 中图分类号: P627

Identification and new discovery of Qiansxuilan fault belt in Gaudeanmus area, Namibia based on the multi-source remote sensing data

  • 摘要: 遥感影像因其可直观显示地质构造形迹的物理特征及地表形态,弥补野外点线观测的局限性,在成矿环境识别及资源评价领域受到众多地学工作者的青睐。以纳米比亚欢乐谷白岗岩型铀成矿区为研究区,基于ETM+、Radarsat-2多源遥感数据,通过开展彩色合成、纹理信息提取、光学和雷达信息融合等图像信息增强,从地层、岩体、构造、地形、水系、植被等方面构建了千岁兰断裂带遥感解译标志,如岩体、岩层被切割、错开或呈穹窿状,地貌为破碎的山体垭口形态或地形切割强烈破碎的深沟,发育硅化、高岭土化、钾化、方解石化、绿泥石化蚀变现象等。基于构建的遥感解译标志和断裂识别方法,识别出了区内部分出露、部分隐伏、规模最大且最重要的千岁兰控矿断裂,创新性提出了千岁兰断裂在区内并非为1组断裂,而是由北部、中部、南部3组断裂组成的断裂带。结合野外出露断裂判别特征和控矿作用分析,验证了千岁兰断裂带的真实存在,且正是该断裂带控制着区内含铀白岗岩和铀矿化的产出。

     

  • 图 1  欢乐谷地区铀矿地质简图(据文献[8]修改)

    Figure 1.  Uranium geological diagram of Gaudeanmus area, Namibia

    图 2  ETM+和RadarSat-2遥感数据处理流程

    Figure 2.  Flow chart of remote sensing data processing of ETM+ and RadarSat-2

    图 3  研究区千岁兰断裂带遥感地质解译图(以ETM+752遥感影像为底图)

    Figure 3.  Interpretation map of Qinsuilan fault zone based on the technology of remote sensing geology in the study area

    图 4  基于ETM+752遥感影像(a)和RadarSat-2纹理提取影像(b)的千岁兰北部断裂带解译图

    Figure 4.  Interpretation map of the northern fault zone of Qiansuilan based on the ETM+752 image (a)and RadarSat-2 texture image (b)

    图 5  基于ETM+752遥感影像(a)和基于RadarSat-2纹理信息与ETM+752融合(b)的千岁兰中部断裂带解译图

    Figure 5.  Interpretation map of the middle fault zone of Qiansuilan based on the ETM+752 image(a)and fusion image of RadarSat-2 texture and ETM+752 image(b)

    图 6  基于ETM+2纹理影像(a)和RadarSat-2纹理影像(b)的千岁兰南部断裂带解译图

    Figure 6.  Interpretation map of the southern fault zone of Qiansuilan based on the ETM+2 texture image(a)and the RadarSat-2 texture image(b)

    图 7  千岁兰北部断裂带野外验证

    a.断裂构造破碎带;b.沿断裂侵入的方解石脉;c.D期富铀白岗岩近景图

    Figure 7.  Field validation of the northern fault zone of Qiansuilan: Fractured shatter zone (a), intrusion calcite veins along the fault (b), close up view of alaskite of stage D rich in uranium (c)

    图 8  千岁兰中部断裂带野外验证

    a.褶曲石英岩层;b.断裂带摩擦镜面,热现象明显;c.断裂面中夹持的断层泥

    Figure 8.  Field validation of the middle fault zone of Qiansuilan: Folded quartzite(a), slickenside of fault zone (b), fault clay clamped in the fault surface(c)

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  • 收稿日期:  2019-07-22

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