Metallogenic regularity of Meso-Cenozoic stratabound glutenite-type Cu-Pb-Zn deposits in the southwestern Tianshan Mountains

LIU Zengren; ZHU Hongying; JIA Runxing; SHUAI Lei; TANG Hu

doi:10.12090/j.issn.1006-6616.20222803

Volume 28 Issue 1

Feb. 2022

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LIU Zengren, ZHU Hongying, JIA Runxing, et al., 2022. Metallogenic regularity of Meso-Cenozoic stratabound glutenite-type Cu-Pb-Zn deposits in the southwestern Tianshan Mountains. Journal of Geomechanics, 28 (1): 50-66. DOI: 10.12090/j.issn.1006-6616.20222803

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Metallogenic regularity of Meso-Cenozoic stratabound glutenite-type Cu-Pb-Zn deposits in the southwestern Tianshan Mountains

doi: 10.12090/j.issn.1006-6616.20222803

LIU Zengren^{1, 2
,},
ZHU Hongying^{1, 2},
JIA Runxing^{1, 3},
SHUAI Lei^{1, 2},
TANG Hu^{1, 2}

1.
China Non-ferrous Metals Resource Geological Survey, Beijing 100012, China
2.
Xinjiang Institute of Geological Survey, China Non-ferrous Metals Resource Geological Survey, Urumqi 830011, Xinjiang, China
3.
Innovation Laboratory of Mine, Environment and Mineral, China Non-ferrous Metals Resource Geological Survey, Beijing 100012, China

Funds:

the Project of China Geological Survey DD20160001

More Information

Received: 2021-09-30
Revised: 2021-12-10

Abstract

Abstract

The southwestern Tianshan Mountains is an important producing area of the Meso-Cenozoic stratabound glutenite-type Cu-Pb-Zn deposits in Xinjiang. Sareke copper mine, Wulagen lead-zinc mine, Huayuan copper mine and Jiashi copper mine are the representative deposits, which all occur in the red bed basin on the edge of the uplift denudation area and are strictly controlled by strata. The lower part of the ore-bearing basin is composed of coal-bearing hydrocarbon-generating rocks, the middle part is well-permeable glutenites as the Cu-Pb-Zn reservoir, and the overlying layer is a sealed cap formed by gypsum rocks and mudstones, showing the ore-forming characteristics of co-enrichment of Cu-Pb-Zn-Uranium-coal-natural gas in the same basin. In this paper, we summarized the sedimentary-tectonic evolution of these ore-bearing basins and the characteristics of ore-bearing layers, and analyzed the ore-controlling conditions and metallogenic characteristics of typical copper, lead and zinc deposits. Combining with comparative analysis, we summarized the regional metallogenic regularity of the Meso-Cenozoic glutenite-type Cu-Pb-Zn deposit, and hold the view that organic matter is closely related to Cu-Pb-Zn mineralization. Moreover, it is inferred that Cu-Pb-Zn-lean ore bodies were formed over the original source layer in the uplift caused by the superimposition of oilfield brine; Cu-Pb-Zn-rich ore bodies were formed by the superimposition of deep-source ore-forming fluids from the Himalayan fault structure. The metallogenic model of the middle Cenozoic stratabound glutenite-type Cu-Pb-Zn deposits in the southwestern Tianshan Mountains provides a basis for the exploration of the known mines in their deep and edge, and also provides guidance for the regional prospecting work.
- ore bearing horizon,
- sedimentary facies,
- oilfield brine,
- organic matter,
- glutenite-type Cu-Pb-Zn deposit,
- stratabound deposits,
- sedimentary tectonic evolution,
- southwestern Tianshan Mountains

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