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《Geology and Mineral Resources of South China》 2005-01
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Relationship between magmatism and polymetal mineralization in Dongwuqi area,Inner Mongolia

JIN Yan~1,LIU Yu-tang~1,XIE Yu-ling~2(1.Institute of Geology,Inner Mongolia Bureau of Nonferrous Geology and Exploration,Hohhot 010010, China; 2. Department of Resource Engineering,Beijing University of Science and Technology,Beijing 100083,China)  
Intrusions,especially Late Hercynian and Early Yanshanian intrusions,are widespread in Dongwuqi area,Inner Mongolia. Late Hercynian intrusions are dominated by acid granites with small amount of diorite. Early Yanshanian intrusions are mainly adamellite,biotite K-feldspar granite with small amount of granodiorite. Pb-Zn mineralization in the studying area is usually related to adamellite,and Fe-Cu mineralization to biotite granite,while Cu mineralization to diorite or diorite porphyrite. The contents of Pb,Zn,W,Sn and Ag in porphyry bodies related to mineralization are several times higher than those of Виноградов value. So,there are excellent condition for prospecting phorphyry ore deposits in this area.
【Fund】: 内蒙古自治区地质勘查重大科技项目(200415003).
【CateGory Index】: P588.12;P618.4
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