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2015, 34(2) 379-384 DOI:
ISSN: 1004-5589 CN: 22-1111/P |
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Geological characteristics and geophysical prospecting signs of Daoga gold mining area in Inner Mongolia |
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WANG Cheng-Yang, WEI Lie-Min, WANG Xiao-Wu, XU Ai-Jun, WANG Wen-Xu, WANG Ke-Yong |
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1. College of Earth Sciences��Jilin University��Changchun 130061��China; 2. Sichuan Huayuan Mining Exploration Development Co. ��LTD��Chengdu 610072��China; 3. No. 8 Exploration Institute of Geology and Mineral ��esources����izhao 276826��Shandong��China; 4. China Gold Group Haigou Mining Co. ��LTD��Antu 133611��Jilin��China; 5. No. 208 Geological Party��CNNC��Baotou 014010��Inner Monglia��China |
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Abstract��
Daoga gold mining area is located in the east section of Beishan metallogenic belt��Ejina County�� Inner Mongolia�� The orebody of this area occurred in shallow metamorphic clastic rocks of Suishishan Formation and Hercynian diorite��and the distributions of the orebody are strictly controlled by NE and EW fault structures�� Gold- bearing quartz vein is the main mineralization type in this area��and the ore is mainly formed by brecciated sulfide- rich quartz veins and tourmaline- quartz veins in type��and the genesis of gold mineralization of this area is belong to mesothermal vein type�� Based on the analysis of IP anomaly of vein��and vein ���� apparent chargeability of anoma- ly range of is from 5% to 9% and apparent resistivity is from 50 ٷm to 300 ٷm��which is considered the IP anomaly with low resistivity and high polarization in the surveyed area as the effective geophysical ore- hunting indication�� |
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Keywords��
Daoga gold mining area
quartz vein type
geological characteristic
geophysics
induced polari- zation
Inner Mongolia
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