Geological characteristics and analysis of ore potential of China-Mongolia-Russia Economic Corridor

ZHANG Fuxiang; ZHAO Sha; WANG Fengxiang; LIU Cheng; NIE Fengjun; ZHAO Yuanyi

2020 Vol. 39, No. 2-3

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ZHANG Fuxiang, ZHAO Sha, WANG Fengxiang, LIU Cheng, NIE Fengjun, ZHAO Yuanyi. Geological characteristics and analysis of ore potential of China-Mongolia-Russia Economic Corridor[J]. Geological Bulletin of China, 2020, 39(2-3): 365-386.

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ZHANG Fuxiang, ZHAO Sha, WANG Fengxiang, LIU Cheng, NIE Fengjun, ZHAO Yuanyi. Geological characteristics and analysis of ore potential of China-Mongolia-Russia Economic Corridor[J]. Geological Bulletin of China, 2020, 39(2-3): 365-386.

Geological characteristics and analysis of ore potential of China-Mongolia-Russia Economic Corridor

1.
College of Resource Science, Hebei GEO University, Shijiazhuang 050031, Hebei, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Geological staff University of Hebei Province, Shijiazhuang 050081, Hebei, China
4.
The Center of Land and Recourse Exploration, Hebei Bureau of Geology and Mineral Exploration, Shijiazhuang 050081, Hebei, China

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Corresponding author: ZHAO Yuanyi, yuanyizhao2@sina.com

Received Date: 21 March 2019

Revised Date: 17 September 2019

Publish Date: 15 March 2020

Abstract

Abstract

The purpose of this study is to enhance the knowledge of the distribution and acquire information on research and exploration of ore resources in the hinterland of the corridor.Preliminary study shows that China-Mongolia-Russia Economic Corridor can be divided into four metallogenic zones:Sino-Korea metallogenic zone, Ural-Mongolian metallogenic zone, Siberian metallogenic zone and European metallogenic zone.Among them, the Sino-Korean and Ural-Mongolian metallogenic belts are characterized by wide distribution of large-scale Cu-Au, Ag, Pb-Zn and Sn-polymetallic deposits, the European metallogenic zone is characterized by enrichment of Ni-Cu, Fe, Au and Pb-Zn deposits, and the Siberian metallogenic sections are characterized by wide distribution of the Ni-Cu-PGE, Nb-polymetalland diamond deposits.A study of ore-forming pedigree shows that the different tectonic units in this region mainly underwent six stages of crust evolution from the Archaean to the Cenozoic, corresponding to six periods of ore deposits:the TIF-type Fe-deposits formed in Precambrian, the porphyry Cu-Au and magmatic Vi-bearing titanomagnetite deposits formed in Caledonian, the hydrothermal vein-type Au deposits related to the intrusions, Sn-polymetal mineralization, Au, Ag-Pb-Zn, Sn-W and other polymetallic deposits formed in Yanshannian period and some hydrothermal deposits formed in Cenozoic.Main ore species in eastern and central part of the corridor are Cu, Mo, Au, Ag, Pb, Zn and diamond.The main types of deposits are porphyry, hydrothermal vein, LS epithermal, alluvial, and marine volcanic rock types, and main ore species in the western part of the corridor are Fe-Cu, Ni-Cu, Pb-Zn, with the main deposits being of IOCG, porphyry and hydrothermal vein types.
- geological features /
- metallogenic zone /
- ore potential /
- China-Mongolia-Russia economic corridor /
- the Belt and Road

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