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YANG Zhengkun, YANG Yang, ZHANG Zhongkun, LIN Bin, HE Jian, ZHANG Zebin, GAO Futai, TANG Xiaoqian, TANG Pan, QI Jing. Geochemistry of pyrrhotite in the Jiama deposit, Tibet and its relationship with gold enrichment and precipitation[J]. GEOLOGY IN CHINA, 2022, 49(4): 1198-1213. DOI: 10.12029/gc20220411
Citation: YANG Zhengkun, YANG Yang, ZHANG Zhongkun, LIN Bin, HE Jian, ZHANG Zebin, GAO Futai, TANG Xiaoqian, TANG Pan, QI Jing. Geochemistry of pyrrhotite in the Jiama deposit, Tibet and its relationship with gold enrichment and precipitation[J]. GEOLOGY IN CHINA, 2022, 49(4): 1198-1213. DOI: 10.12029/gc20220411

Geochemistry of pyrrhotite in the Jiama deposit, Tibet and its relationship with gold enrichment and precipitation

Funds: 

National Key Research and Development Program of China 2018YFC0604101

Basic Research Fund of Institute of Mineral Resource, Chinese Academy of Geological Sciences KJ2102

Basic Research Fund of Institute of Mineral Resource, Chinese Academy of Geological Sciences KK2017

Sciences and Technical Plan from Tibet XZ201901-GB-24

the National Natural Science Foundation of China 41902097

the project of China Geological Survey DD20190167

More Information
  • Author Bio:

    YANG Zhengkun, male, born in 1983, engineer, engaged in the study of exploration and management of mine; E-mail: yzk-0902@163.com

  • Corresponding author:

    YANG Yang, male, born in 1992, doctor candidate, engaged in the study of exploration and metallogeny; E-mail: nickyang87@126.com

  • Received Date: June 20, 2020
  • Revised Date: October 09, 2020
  • Available Online: September 25, 2023
  • This paper is the result of mineral exploration engineering.

    Objective 

    As one of the most important porphyry metallogenic systems in Gangdese metallogenic belt in Tibet, Jiama has a four in one orebody structure of porphyry, skarn, hornfels, and vein gold ore-body, forming riched minerals and diverse metal mineralization. Pyrrhotite is one of the important metal minerals, and its mineral geochemistry and relationship with gold mineralization are still obscure.

    Methods 

    The mineralogy and geochemistry of pyrrhotite in different occurrences of the Jiama porphyry system are the main objects for this paper according to detailed field geological survey, petrography, and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) analysis.

    Results 

    The results show that pyrrhotite is obviously enriched in Co, Ni, Cu, Zn, Ge, and Se, and weakly enriched in Pb, Bi, Sb, Te, Ag, and As, and low content of Mo, Cd, In, Sn, Ba, W, Au, Tl, Th, U, relatively. Moreover, the pyrrhotite from skarn has a high ratio of Co/Ni, represent the its magmatic-hydrothermal genesis, while the pyrrhotite hosted in hornfels shows sedimentary characteristics.

    Conclusions 

    The variation of contents of Cu, Zn, and Pb in pyrrhotite are related to the spatial mineralization in the Jiama deposit. The massive pyrrhotite in skarn is closely related to gold mineralization and the gold is mainly anhedral or irregular free gold occurring in the cavity and boundary of pyrrhotite grains. The enrichment and precipitation of gold could be related to bismuth-rich melts in the ore-fluids.

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