朱裕振, 张文艳, 高志军, 汝亮. 0: 分布式三维广域电磁法在李屯厚覆盖区富铁矿勘查中的应用. 地质通报. DOI: 10.12097/gbc.2022.09.023
    引用本文: 朱裕振, 张文艳, 高志军, 汝亮. 0: 分布式三维广域电磁法在李屯厚覆盖区富铁矿勘查中的应用. 地质通报. DOI: 10.12097/gbc.2022.09.023
    Yuzhen ZHU, Wenyan ZHANG, Zhijun GAO, Liang RU. 0: Application of distributed 3D wide field electromagnetic method in the exploration of rich iron ore in the thick covered area of Litun. Geological Bulletin of China. DOI: 10.12097/gbc.2022.09.023
    Citation: Yuzhen ZHU, Wenyan ZHANG, Zhijun GAO, Liang RU. 0: Application of distributed 3D wide field electromagnetic method in the exploration of rich iron ore in the thick covered area of Litun. Geological Bulletin of China. DOI: 10.12097/gbc.2022.09.023

    分布式三维广域电磁法在李屯厚覆盖区富铁矿勘查中的应用

    Application of distributed 3D wide field electromagnetic method in the exploration of rich iron ore in the thick covered area of Litun

    • 摘要: 为了揭示李屯厚覆盖区富铁矿深部精细地质构造,开展了分布式三维广域电磁探测,应用高阶2n序列伪随机信号,一次能够发射49个频率并同时接收,实现分布式滚动测量,获得地下2000m以浅地电特征,并对地下地质结构进行精细解释,构建了重点研究区的三维地质模型,解释结果与已有的地震和钻探信息吻合度较高,为重磁联合反演提供有效约束,结合成矿规律圈定新的找矿靶区。结果表明,分布式三维广域电磁法是获取厚覆盖地区深部精细地质结构的有效探测方法,具有良好的应用前景。

       

      Abstract: To reveal the fine geological structure in the deep Litun iron-rich deposit in the thick coverage area, distributed three-dimensional wide field electromagnetic detection was carried out. It uses high-order 2n sequence pseudo-random signal, can transmit 49 frequencies at a time and receive at the same time, realize distributed rolling measurement, and obtain the geoelectric characteristics of 2000m underground. Based on this, a detailed interpretation of the underground geological structure was carried out, and a three-dimensional geological model of the key research area was constructed. The interpretation results were in good agreement with the existing seismic and drilling information. It provides effective constraints for gravity-magnetic joint inversion and delineates new prospecting targets in combination with metallogenic laws. The results show that the distributed three-dimensional wide field electromagnetic method is an effective detection method to obtain the deep fine geological structure in the thick coverage area and has a good application prospect.

       

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