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

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

  • 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

    • Fund Project: Supported by National Natural Science Foundation of China (No. U1403292) and National Science and Technology Support Program (No. 2015BAB05B04)
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  • 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:  06 November 2016
Revised Date:  24 November 2017
Publish Date:  25 February 2018
    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.

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