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Volume 30 Issue 1
Jan 2019
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Journal of Earth Science  > 2019  >  30(1): 131-141.
Huang Chaowen, Du Gaofeng, Jiang Huajun, Xie Jianfeng, Zha Daohan, Li Huan, Lai Chun-Kit. Ore-Forming Fluids Characteristics and Metallogenesis of the Anjing Hitam Pb-Zn Deposit in Northern Sumatra, Indonesia. Journal of Earth Science, 2019, 30(1): 131-141. doi: 10.1007/s12583-019-0859-z
Citation: Huang Chaowen, Du Gaofeng, Jiang Huajun, Xie Jianfeng, Zha Daohan, Li Huan, Lai Chun-Kit. Ore-Forming Fluids Characteristics and Metallogenesis of the Anjing Hitam Pb-Zn Deposit in Northern Sumatra, Indonesia. Journal of Earth Science, 2019, 30(1): 131-141. doi: 10.1007/s12583-019-0859-z
shu

Ore-Forming Fluids Characteristics and Metallogenesis of the Anjing Hitam Pb-Zn Deposit in Northern Sumatra, Indonesia

doi: 10.1007/s12583-019-0859-z
  • 1.

    Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha 410083, China

  • 2.

    Geological Survey of Anhui Province, Hefei 230001, China

  • 3.

    School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China

  • 4.

    Research Institute of Hunan Provincial Nonfenous Metals Geological Exploration Bureau, Changsha 410015, China

  • 5.

    Hunan Key Laboratory of Land Resources Evaluation and Utilization, Changsha 410015, China

  • 6.

    Faculty of Science, Universiti Brunei Darussalam, Gadong BE1410, Brunei Darussalam

  • 7.

    Centre of Excellence in Ore Deposits(CODES), University of Tasmania, Hobart, Tasmania 7001, Australia

More Information
  • Corresponding author: Gaofeng Du
  • Received Date: 08 Dec 2017
  • Accepted Date: 30 May 2018
  • Publish Date: 01 Feb 2019
    Abstract
  • The Anjing Hitam Pb-Zn deposit in northern Sumatra (Indonesia) is one of the largest Pb-Zn deposits in the region. The stratiform orebodies are mainly hosted in the middle member of the Carboniferous-Permian Kluet Formation of the Tapanuli Group. Mineral paragenesis and crosscutting relationships suggest a two-stage Pb-Zn mineralization:(Ⅰ) sedimentary and (Ⅱ) hydrothermal mineralization. Ore-related calcite from both stages Ⅰ and Ⅱ contains mainly liquid-and gas-liquid two-phase-type fluid inclusions (FI). For stage Ⅰ ore-forming fluids, FI homogenization temperatures (Th) are 105 to 199℃, and the salinities are 9.6 wt.% to 16.6 wt.% NaCleqiv, reflecting low temperature and medium-low salinity; whereas in stage Ⅱ, the Th (206 to 267℃) and salinity (19.0 wt.% to 22.5 wt.% NaCleqiv) are considerably higher. Fluid inclusion and C-O isotope characteristics suggest that the stage Ⅰ ore-forming fluids were mainly derived from a mixture of seawater and magmatic fluids (probably from deep-lying plutons), whereas the stage Ⅱ ore-forming fluids were likely magmatic-derived with wall rock input. We propose that the Anjing Hitam deposit was a Carboniferous exhalative sedimentary (SEDEX) deposit overprinted by the Pleistocene vein-style magmatic-hydrothermal mineralization.

     

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