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Geophysical-geochemical anomalies in Buhangte area of Inner Mongolia and their prospecting effects |
GAO Si-Xin1, WU Hong-Wei2, ZHAO Qiang3, WANG Lu-Lin2, ZHANG Xue-Zhong2 |
1. Exploration & Development Bureau of Geology & Mineral Resources of Ningxia, Yinchuan 750021, China; 2. No. 3 Geological Survey Institute, Henan Bureau of Geo-exploration and Mineral Development, Xinyang 464000, China; 3. Ningxia Institute of Geological Survey, Yinchuan 750021, China |
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Abstract Along the third grade Cu-Mo-Pb-Zn-Ag-Au-Ni-Cr-Co metallogenic belt in Dong Ujimqin Banner-northern Da Hinggan Mountains region of Inner Mongolia, 1:50, 000 soil survey has revealed that there exist Ag, Pb and Zn mesothermal-epithermal element anomalies which are distributed in the semi-ring form around high-temperature elements Sn, W and Mo. The anomalies have high intensity and obvious compositional zoning. The 1:10, 000 soil anomalies delineated by anomaly verification are distributed similar to the above anomalies, but with higher intensity; the concentration centers of Pb, Zn and Ag anomalies indicate the locations of the shallowly-covered Pb-Zn orebodies. The low-resistivity and high-polarizability circular planar anomalies corresponding to the soil anomalies indicate the existence of polarized bodies. It is inferred that there exists a concealed granite-porphyry body in the depth, and this rock body as well as the depth of its endo-and exo-contact zones has fairly promising prospecting potential. Guided by the porphyry metallogenic theory, the authors further found a number of shallowly-covered lead-zinc orebodies, concealed silver orebodies and molybdenum orebodies, and summarized the geological, geophysical and geochemical indicators in search for ore deposits.
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Received: 28 June 2013
Published: 10 August 2014
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