STRUCTURAL CONDITIONS OF COPPER-POLYMETALLIC MINERALIZATION IN THE SOUTHEAST SECTION OF DAXINANLING MOUNTAINS
ZHANG Yong-zheng1, LI Xiu-rong2, YANG Hong-zhi2, SHAO Jun2
1. Inner Mongolia Geological Survey, Jining 021000, Inner Mongolia, China; 2. Shenyang Institute of Geology and Mineral Resources, Shenyang 110032, China
Abstract：The southeast section of Daxinganling Mts., covering the east region of Inner Mongolia, is an important component of the Daxinganling metallogenetic belt, which involves three structural layers, i. e. Precambrian layer, Paleozoic layer and Mesozoic layer. The fault systems of the structural layers form the structural framework characterized by equal-interval and rhombus. The regional structures control copper-polymetallic mineralization in zone, block, knot, spot and margin. Different forms of structures result in the forming of various genetic types of deposits.
张永正, 李秀荣, 杨宏智, 邵军. 大兴安岭东南段铜多金属成矿构造条件[J]. 地质与资源, 2007, 16(1): 38-41.
ZHANG Yong-zheng, LI Xiu-rong, YANG Hong-zhi, SHAO Jun. STRUCTURAL CONDITIONS OF COPPER-POLYMETALLIC MINERALIZATION IN THE SOUTHEAST SECTION OF DAXINANLING MOUNTAINS. GEOLOGY AND RESOURCES, 2007, 16(1): 38-41.
2007, Vol. 16 
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