Geological setting, spatiotemporal distribution of predominant metal deposits in eastern section of China, Mongolia and Russia

LIU Jinlong; LI Zhumin; ZHOU Yongheng; DONG Cunjie

doi:10.12029/gc20230215001

2025 Vol. 52, No. 3

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LIU Jinlong, LI Zhumin, ZHOU Yongheng, DONG Cunjie. 2025. Geological setting, spatiotemporal distribution of predominant metal deposits in eastern section of China, Mongolia and Russia[J]. Geology in China, 52(3): 945-971. doi: 10.12029/gc20230215001

Citation:

LIU Jinlong, LI Zhumin, ZHOU Yongheng, DONG Cunjie. 2025. Geological setting, spatiotemporal distribution of predominant metal deposits in eastern section of China, Mongolia and Russia[J]. Geology in China, 52(3): 945-971. doi: 10.12029/gc20230215001

Geological setting, spatiotemporal distribution of predominant metal deposits in eastern section of China, Mongolia and Russia

1.
Shenyang Center, China Geological Survey, Shenyang 110000, Liaoning, China

Fund Project: Supported by the project of China Geological Survey (No.DD20221806).

More Information

Author Bio: LIU Jinlong, male, born in 1988, senior engineer, mainly engaged in regional geological mineral survey and research; E-mail: liujinlong0815@yeah.net
Corresponding author: LI Zhumin, male, born in 1983, senior engineer, mainly engaged in northeast Asian regional geological mineral survey and research; E-mail: 45569520@qq.com.

Received Date: 15 February 2023

Revised Date: 15 May 2023

Publish Date: 25 May 2025

Abstract

Abstract

This paper is the result of geological survey engineering.
Objective
The eastern segment of China–Mongolia–Russia has a complex geological evolution history with strong mineralization. Thus, it is of great significance to enhance the study about cross−boundary mineralization and, particularly, the summary of region-wide mineralization rules for improving the level of regional basic geological research and ore exploration.
Methods
By compiling all kinds of geological data, we disentangle the metallogenic geological features, resource endowment, temporal and spatial distribution of ore deposits, metallogenic background and so on.
Results
Within the study area, 10 super−large ore deposits, 33 large ore deposits, 55 medium ore deposits, and numerous small ore deposits (and occurrences) were proved or discovered. In general, it can be divided into the deposits related Precambrian tectonic system, the deposits related Paleo–Asian Ocean tectonic system, the deposits related Mongolia–Okhotsk tectonic system, and the deposits superimposed by the Mongolia–Okhotsk Ocean and Paleo–Pacific tectonic system.
Conclusions
The spatial and temporal distribution features of regional ore deposits are obvious: The most important deposits formed in various periods, including the Archean Fe deposits distributed in the West Aldan–Sutam area, the Paleoproterozoic Cu–Fe–Ti deposits distributed in the Udokan–DyosLeglier area and the Neoproterozoic Pb–Zn deposits distributed in the Baikal–Muya tectonic belt, the Cambrian–Silurian Fe–Zn–Ti deposits distributed in the Yenisey–Transbaikalian tectonic belt, the Carboniferous Au deposits distributed in the Baikal–Patom tectonic belt, the Triassic Cu and Mo deposits distributed in the Orhon–Selenge area and the Late Permian–Early Triassic Fe deposits in the Angara–Ilim area, and the Middle Jurassic–Cretaceous Au–Pb–Zn–W–Mo deposits distributed in the Mongolia–Okhotsk tectonic belt and its surrounding areas.
- metal deposit /
- Au–Pb–Zn–W–Mo minerals /
- geological setting /
- Siberian Platform /
- the Paleo–Asian Ocean /
- the Mongolia–Okhotsk Ocean /
- geological survey engineering

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