| Citation: |
WANG Zhong-lian, WANG Yong-guo, WANG Zhi-mao, LU Xue-bin. JOINT PROSPECTING OF GROUND MAGNETIC SURVEY DATA INVERSION AND BOREHOLE MAGNETIC SURVEY: A Case Study of Galinge Fe-polymetallic deposit[J]. Geology and Resources, 2020, 29(1): 61-67.
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JOINT PROSPECTING OF GROUND MAGNETIC SURVEY DATA INVERSION AND BOREHOLE MAGNETIC SURVEY: A Case Study of Galinge Fe-polymetallic deposit
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Abstract
The Quaternary overburden in Galinge iron polymetallic orefield in Qinghai Province is nearly 200 m. The deposit is dominated by iron ore, associated with polymetallic ores such as copper, cobalt, lead and zinc. Magnetic prospecting is the most direct and effective method. Based on the analysis of ground magnetic survey data, the magnetic bodies are found in deep part with the 2.5-D inversion modeling. The processing and analysis of the borehole three-component magnetic survey data provide a basis for borehole layout and a guide for drilling construction. Good geological results have been achieved in deep prospecting.
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References
[1] 吴小霞, 保广英, 伊有昌, 等.青海省尕林格富铁矿床地质特征及成因探讨[J].黄金科学技术, 2007, 15(4):36-40. doi: 10.3969/j.issn.1005-2518.2007.04.008 [2] 卫岗, 王进文, 王永国, 等.青海尕林格Ⅴ矿群磁异常特征分析[J].地质与资源, 2012, 21(5):478-482. doi: 10.3969/j.issn.1671-1947.2012.05.012 [3] 朱朝吉, 周肇武, 刘天佑, 等.高精度磁测找矿效果:以青海尕林格矿区为例[J].地质与勘探, 2011, 47(2):277-283. [4] 王永国, 马晓光, 王进文, 等.井地联合磁测找矿效果——以青海尕林格Ⅺ矿区为例[J].地质与资源, 2014, 23(1):92-96. doi: 10.3969/j.issn.1671-1947.2014.01.015 [5] 王庆乙, 李学圣, 徐立忠.高精度井中三分量磁测是矿山深部找矿的有效手段[J].物探与化探, 2009, 33(3):235-239, 244. -
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WANG Zhong-lian, WANG Yong-guo, WANG Zhi-mao, LU Xue-bin. JOINT PROSPECTING OF GROUND MAGNETIC SURVEY DATA INVERSION AND BOREHOLE MAGNETIC SURVEY: A Case Study of Galinge Fe-polymetallic deposit[J]. Geology and Resources, 2020, 29(1): 61-67.
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Figure 1.
Magnetic anomaly contour map of Galinge No. Ⅱ ore block
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Figure 2.
Magnetic anomaly by reduction-to-the-pole contour map of Galinge No. Ⅱ ore block
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Figure 3.
2.5-D forward calculation along exploratory line No. 24
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Figure 4.
Residual anomaly along exploratory line No. 24
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Figure 5.
2.5-D inversion result along exploratory line No. 24
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Figure 6.
Three-component magnetic survey curves of borehole ZK2405
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Figure 7.
Geological profile along exploratory line No. 24