Geological characteristics and sulfur and lead isotopes of the Kanling lead-zinc deposit, Southern Tianshan Mountains

YANG Bin; CHEN Zhengle; ZHANG Qing; ZHOU Zhenju; HAN Fengbin; ZHANG Wengao; MA Ji; ZHANG Tao

doi:10.12029/gc20180113

GEOLOGY IN CHINA > 2018 > 45(1): 155-167. > DOI: 10.12029/gc20180113

YANG Bin, CHEN Zhengle, ZHANG Qing, ZHOU Zhenju, HAN Fengbin, ZHANG Wengao, MA Ji, ZHANG Tao. Geological characteristics and sulfur and lead isotopes of the Kanling lead-zinc deposit, Southern Tianshan Mountains[J]. GEOLOGY IN CHINA, 2018, 45(1): 155-167. DOI: 10.12029/gc20180113

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Geological characteristics and sulfur and lead isotopes of the Kanling lead-zinc deposit, Southern Tianshan Mountains

YANG Bin^{1, 2, 3,},
CHEN Zhengle^{1, 2, ,},
ZHANG Qing²,
ZHOU Zhenju²,
HAN Fengbin²,
ZHANG Wengao²,
MA Ji¹,
ZHANG Tao¹

1.
School of Earth Science, East China University of Technology, Nanchang 330013, Jiangxi, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
South Jiangxi Geological Survey Party of JBEDGMR, Ganzhou 341000, Jiangxi, China

Funds:

National Natural Science Foundation of China U1403292

National Science and Technology Support Program 2015BAB05B04

More Information

Author Bio:
YANG Bin, male, born in1990, master candidate, majors in the study of geology; E-mail:jxgzyb@163.com
Corresponding author:
CHEN Zhengle, male, born in1967, professor, mainly engages in the study of orefield structure; E-mail:chenzhengle@263.net
Received Date: November 05, 2016
Revised Date: November 23, 2017
Available Online: September 25, 2023

Graphical Abstract

Abstract

Abstract

The Kanling lead-zinc deposit is one of the typical lead-zinc deposits in south Tianshan orogen, Xinjiang. It is located in the Kalpin uplift belt on the northwestern margin of the Tarim plate. Geological survey and isotope studies show that the host rocks of the deposit with epigenetic genesis are Upper Cambrian-Ordovician carbonate rocks, and the orebodies exhibit veined, stratoid and lenticular forms, mainly controlled by the fault and strata. Galena and sphalerite are the main ore minerals, with weak wall rock alteration. The characteristics of the sulfur isotope (in the range of -1‰-12.2‰) imply that the sources of sulfur was mainly derived from the deep mantle and sedimentary strata, the Pb isotopic composition of the ore is more homogeneous, and the ²⁰⁶Pb/²⁰⁴Pb ratios range from 17.262 to 17.269, ²⁰⁷Pb/²⁰⁴Pb from 15.571 to 15.675, and ²⁰⁸Pb/²⁰⁴Pb from 38.062 to 38.396; the ore-forming metals were mainly derived from the sedimentary strata as compared with the Pb isotopic characteristics of the ore and the host rocks. Geological and geochemical characteristics of the deposit indicate that the Kanling lead-zinc deposit is a MVT deposit, which is hosted in the platform carbonate rocks.
- deposit geology,
- sulfur and lead isotope,
- lead?zinc deposit,
- South Tianshan orogen

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References (60)

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Geological characteristics and sulfur and lead isotopes of the Kanling lead-zinc deposit, Southern Tianshan Mountains