Structural ore−controlling mechanism of the Qingshan lead−zinc deposit in northwestern Guizhou, China and its implications for deep prospecting

SONG Danhui; HAN Runsheng; WANG Feng; WANG Mingzhi; HE Zhi; ZHOU Wei; LUO Da

doi:10.12029/gc20200828002

2024 Vol. 51, No. 2

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Article navigation > Geology in China > 2024 > 51(2): 399-425

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SONG Danhui, HAN Runsheng, WANG Feng, WANG Mingzhi, HE Zhi, ZHOU Wei, LUO Da. 2024. Structural ore−controlling mechanism of the Qingshan lead−zinc deposit in northwestern Guizhou, China and its implications for deep prospecting[J]. Geology in China, 51(2): 399-425. doi: 10.12029/gc20200828002

Citation:

SONG Danhui, HAN Runsheng, WANG Feng, WANG Mingzhi, HE Zhi, ZHOU Wei, LUO Da. 2024. Structural ore−controlling mechanism of the Qingshan lead−zinc deposit in northwestern Guizhou, China and its implications for deep prospecting[J]. Geology in China, 51(2): 399-425. doi: 10.12029/gc20200828002

Structural ore−controlling mechanism of the Qingshan lead−zinc deposit in northwestern Guizhou, China and its implications for deep prospecting

1.
Kunming University of Science and Technology, College of Land and Resources Engineering, Kunming 650093, Yunnan, China
2.
Southwest Institute of Geological Survey, Geological Survey Center for Non−ferrous Mineral Resources, Kunming 650093, Yunnan, China
3.
Yunnan Chihong Zinc and Germanium Co., Ltd., Qujing 655011, Yunnan, China
4.
Guizhou Hongqiao Mining Group Co. LTD, Liupanshui 553000, Guizhou, China

Fund Project: Supported by National natural Science Foundation Project (No.41572060), Projects for Yunling Scholars (2014), Yunnan Engineering Laboratory of Mineral Resources Prediction and Evaluation (YM Lab) (2010) and Geological Process and Mineral Resources Innovation Team (2012).

More Information

Author Bio: SONG Danhui, male, born in 1995, master candidate, major in geological engineering; E-mail: 806798929@qq.com
Corresponding author: HAN Runsheng, male, born in 1964, professor, supervisor of doctor candidates, engaged in research of the dynamics of tectonic ore−forming processes and prognosis of concealed deposit; E-mail: 554670042@qq.com.

Received Date: 28 August 2020

Revised Date: 18 January 2021

Publish Date: 25 March 2024

Abstract

Abstract

This paper is the result of mineral exploration engineering.
Objective
The Qingshan medium−size Pb−Zn deposit is located in the middle of the Weining−Shuicheng metallogenic sub−belt in the southwest margin of the Yangzi Block. The ore−body of the Qingshan deposit is strict controlled by structure and the resource potential is huge.
Methods
Based on the theory and method of orefield geomechanics, this research has revealed the mechanism of structural ore control by the fine survey of large−scale structural profile, the identification of mechanical properties of typical ore−controlling structures in different directions and the screening of structures in different periods and orders, combined with the characteristics of regional tectonic stress field.
Results
The results show that the principal compressive stress direction of the mining area since the Indosinian had changed from NE−SW−trending to NW−SE−trending to NE−SW−trending to near EW−trending, sequentially forming tectonic systems of the early NW tectonic belt, the NE tectonic belt, the late NW tectonic belt and the SN tectonic belt in turn. By the analysis of ore−controlling structure and the discussion of its relationship with mineralization, the metallogenic structural system of the north−east tectonic belt has been determined, and the hierarchical ore−controlling regularity of structure is revealed, it is, the northwest−trending Weining−Shuicheng fault and Weining−Shuicheng anticline are the first−grade ore−controlling structures, which control the distribution of the Weining−Shuicheng metallogenic sub−belt or orefield; The NW−trending faults (F₁ and F₂) derived from the Weining−Shuicheng fault, control the distribution of the deposit or orebody group, and are the second−grade ore−controlling structures in the mining area; The interlayer fracture zones between F₁ and F₂ faults directly control the feature and attitude of orebodies, which is the third−grade ore−controlling structure in the mining area; The joint fissures on the sides of orebodies control the ore−veins, which is the fourth−grade ore−controlling structure.
Conclusions
The regularities of structural classification control are obvious for the Qingshan Pb−Zn deposit, which is mainly controlled by the ore−controlling structures of four grades, and has formed the four types of mineralization styles.
- metallogenic tectonic system /
- ore−controlling mechanism /
- model of tectonic ore control /
- mineral exploration implication /
- Qingshan lead−zinc deposit /
- northwestern Guizhou Province /
- mineral exploration engineering

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