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The application of high precision gravity and magnetic survey to prospecting in coverage area:A case study of the reconnaissance of Weishan iron and copper deposit in Wuwei County |
Min ZHAO, Yong SHENG, Liang-Gang QI |
Anhui Institute of Geophysical and Geochemical Prospecting Techniques, Hefei 230022, China |
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Abstract In the coverage area, it is very difficult to carry out the conventional geological work , whereas the high-precision gravity and magnetic survey methods can quickly and effectively divide the buried faults and determine the rock boundary, which provides important assistance for prospecting in the coverage area. With the Weishan iron-copper deposit reconnaissance in Wuwei County of Anhui Province as an example, the authors divided the faults and determined rock boundary in the pre-investigation area through the processing and analysis of gravity and magnetic anomalies. Combined with geological features, two gravity and magnetic anomalies with large potential for prospecting were screened where a 40 m rich iron orebody with a TFe grade of about 52% and a mFe grade of about 38% was found by drilling. Therefore, the effectiveness of the method is confirmed, and this result also has certain guiding significance for the prospecting work in the eastern marginal coverage area of the Luzong volcanic basin where the investigation area is located.
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Received: 13 March 2019
Published: 28 November 2019
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Geological map in the Weishan area of Wuwei in Anhui province 1—Quaternary system;2—Paleogene system;3—Jurassic Luoling Fm;4—Jurassic Moshan Fm;5—Triassic Dongmaanshan Fm;6—Devonian Wutong Fm;7—Silurian Maoshan Fm;8—Silurian Fentou Fm;9—Quartz syenite;10—Syenite;11—fault;12—Pre-investigation area
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Gravity and magnetic anomaly map of the Luzong area 1—Δg contour;2—gravity high;3—gravity low;4—ΔT negative contour;5—ΔT zero contour;6—ΔT positive contour;7—pre-investigation area
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Bouguer gravity anomaly map in Weishan area
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ΔT apolar anomaly map in Weishan area
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Residual gravity and magnetic anomaly map in Weishan area 1—residual positive magnetic anomaly;2—residual gravity high;3—residual gravity low;4—inferred faults;5—inferred rock mass;6—drilling
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Line 11 2.5D gravity and magnetic inversion profile 1—Quaternary system;2—Triassic middle series;3—Triassic lower series- Permian system;4—Permian Qixia Fm;5—Carboniferous system;6—Devonian system-Silurian system;7—Silurian lower-middle series ;8—Andesiticporphyrite;9—inferred rock mass;10—inferred magnetite ore;11—design drilling and number
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