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Three-dimensional inversion analysis of magnetic data from deep buried iron ore and prediction of prospecting target area |
Yu-Zhen ZHU1, Jian-Ke QIANG2( ), Lin-Fei WANG3, Wen-Yan ZHANG2, Shi-Kun DAI2 |
1. Shandong Coalfield Geological Planning and Investigation Institute, Jinan 250104,China 2. School of Earth Sciences and Information Physics, Central South University, Changsha 410083, China 3. China Aerospace Geophysical and Remote Sensing Center, Beijing 100083, China |
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Abstract The search for deep buried iron deposits is a very complicated exploratory study. The current difficulty is that the ferromagnetic anomalies are small and submerged in large magnetic intrusive rock masses. It may cause large deviations and increase the risk of exploration. With the rapid development of computer technology, large-scale three-dimensional inversion has become a reality. This paper uses GMES-3DI commercialization software to automatically invert the area magnetic data of Qihe-Yucheng area in Shandong Province, and obtains the magnetic susceptibility of underground space in this area. Based on the distribution and combined with the existing geological data of boreholes, the authors revealed the characteristics of the magnetic susceptibility contours with high value traps in the presence of iron ore, with the trap center being about 500 m shallower than the actual orebody position. Based on this feature, the authors used the three-dimensional magnetic susceptibility data retrieved from the exploration area to search for areas with high magnetic anomaly traps in the north-south and east-west directions and, as a result, delineated two relatively reliable prospecting targets.
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Received: 28 April 2019
Published: 28 November 2019
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Corresponding Authors:
Jian-Ke QIANG
E-mail: qiangjianke@163.com
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A sketch of regional geological structure
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Diagram of magmatic rock distribution in the region
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The contours of 1:10,000 high-precision magnetic anomalies on the ground
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A sketch of three-dimensional inversion slices of magnetic data a—distribution of measured data;b—3D inversion susceptibility slicing;c—3D inversion susceptibility horizontal slicing;d—3D inversion susceptibility greater than 0.0105SI
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Three-dimensional inversion of magnetic susceptibility contours of eight horizontal slices
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The susceptibility contours of ZK1 and ZK0701 N-S profiles
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The susceptibility contours of the East-West profile of ZK1 and ZK0701 a—the north-south coordinate is 72196;b—the north-south coordinate is 71776
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Predicts the north-south-west-east susceptibility contour profile of No. 1 anomaly a—the north-south coordinate is 75131;b—the east-west coordinate is 51195
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Predicts the north-south-west-east magnetic susceptibility contour profile of anomaly No. 2 a—the north-south coordinate is 708021;b—the east-west coordinate is 57610
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