Structurally-controlled metallogenic processes in the central and southern Great Xingan mountains
The central and southern Great Xingan mountains are one of the important metallogenic provinces in east China and located in the southeast of Inner Mongolia. On the basis of regional strata,magmatic activities, and geophysical information,this paper discusses the characteristics of regional structure and its constraints on ore deposits in the central and southern Great Xingan mountains. The zoned deformation, the metamorphism and intensive magmatism around the axis of the Great Xingan mountains are the major representation of mantle branch activity. The ore deposits are hosted in ductile- brittle shearing zones and detachment zones of mantle branch structures.
Great Xingan mountains Inner Mongolian mantle- branch structure endogenetic ore deposits
Baode Wang Shuyin Niu Huabin Hu Jianzhen Zhang Aiqun Sun Lijun Guo Shuo Wang Jian Shao
Geological Survey Institute, Shijiazhuang University of Economics, Shijiazhuang 050031, China Inner Mongolia Exploitation Bureau of Geology and Mineral Resources, Hohhot 010020, China Institute of Earth and Space Sciences, Beijing University, Beijing 100871, China
国际会议
第八届国际矿床地质会议(Proceedings of the Eighth Biennial SGA Meeting)
北京
英文
128-131
2005-08-18(万方平台首次上网日期,不代表论文的发表时间)