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J4 ›› 2011, Vol. 19 ›› Issue (2): 18-22.
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HUANG Zhongjun,WANG Guichun,GAO Rong
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Abstract:
Dongwuqi area is located in the northeast of Inner Mongolia,the structural feature is complex and magmatic is activity in this area,polymetallic deposit spread everywhere,it is an important gold,silver,copper,lead,zinc, tungsten and molybdenum mining area.NE,NNE trending faults are ore-controlling structures,the fold and fault provides leading ore structure.The development of continental volcanism-subvolcanic and Mesozoic monzogranite provide the necessary heat and material sources for the forming of mineral.Comprehensive analysis,we think that the area is the favorable area looking for gold,silver,copper and polymetallic deposits which are related to magmatic activity,also it is the favorable position of occurrence of altered rock type and magmatic hydrothermal type polymetallic deposit.
Key words: Magmatism, Tectonic evolution, Polymetallic mineralization, 1017 highland, Inner Mongolia
CLC Number:
P618.51
HUANG Zhongjun,WANG Guichun,GAO Rong. The Relationship between Tectonic,Magmatic Activity and Ploymetallic Ore in Dongwuqi of Inner Mongolia,Take 1017 Highland Mining Area as an Example[J].J4, 2011, 19(2): 18-22.
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http://www.goldsci.ac.cn/EN/Y2011/V19/I2/18
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