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Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization

Received: 26 February 2020     Accepted: 17 March 2020     Published: 8 April 2020
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Abstract

The relationship between mafic intrusion and gold deposits has always received substantial attention. Based on the petrography, mineralogy, and chronology of two mafic intrusion suites exposed in the Funing area, we found that the mafic intrusion suites have closely relationship with gold mineralization. The 255±4.9-Ma U-Pb age of the early mafic intrusion suite is much older than the 218.9±6.4-Ma (MSWD=1.2) U-Pb age of the late mafic intrusion suite. Based on previous studies on former gold mines in the area, it is believed that early mafic intrusion suite appears to have contributed to the early hydrothermal enrichment of gold deposits through the action of water-rock, together with atmospheric precipitation and stratigraphic water. Due to favorable structural conditions during the Indosinian tectonic period, the late basic rock not only extracted metallogenic materials from the stratum but also acted as an important heat source for the metallogenic fluid circulation and mineralization, together with superposed mineralization of frequent tectonic activities on early deposits, finally forming into ore deposits in favorable structures. Therefore, we believe that the mafic intrusion suite in the late period of the region are closely related to the gold mineralization in the region, and it can be used as a prospecting mark for gold deposits in the area.

Published in International Journal of Mineral Processing and Extractive Metallurgy (Volume 5, Issue 1)
DOI 10.11648/j.ijmpem.20200501.12
Page(s) 7-19
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2020. Published by Science Publishing Group

Keywords

Mafic Intrusion, Zirconu-Pb Dating, Gold Deposit

References
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    Pi Qiaohui, Wei Chaowen, Yu Huidong, Lu Di. (2020). Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization. International Journal of Mineral Processing and Extractive Metallurgy, 5(1), 7-19. https://doi.org/10.11648/j.ijmpem.20200501.12

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    ACS Style

    Pi Qiaohui; Wei Chaowen; Yu Huidong; Lu Di. Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization. Int. J. Miner. Process. Extr. Metall. 2020, 5(1), 7-19. doi: 10.11648/j.ijmpem.20200501.12

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    AMA Style

    Pi Qiaohui, Wei Chaowen, Yu Huidong, Lu Di. Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization. Int J Miner Process Extr Metall. 2020;5(1):7-19. doi: 10.11648/j.ijmpem.20200501.12

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  • @article{10.11648/j.ijmpem.20200501.12,
      author = {Pi Qiaohui and Wei Chaowen and Yu Huidong and Lu Di},
      title = {Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization},
      journal = {International Journal of Mineral Processing and Extractive Metallurgy},
      volume = {5},
      number = {1},
      pages = {7-19},
      doi = {10.11648/j.ijmpem.20200501.12},
      url = {https://doi.org/10.11648/j.ijmpem.20200501.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijmpem.20200501.12},
      abstract = {The relationship between mafic intrusion and gold deposits has always received substantial attention. Based on the petrography, mineralogy, and chronology of two mafic intrusion suites exposed in the Funing area, we found that the mafic intrusion suites have closely relationship with gold mineralization. The 255±4.9-Ma U-Pb age of the early mafic intrusion suite is much older than the 218.9±6.4-Ma (MSWD=1.2) U-Pb age of the late mafic intrusion suite. Based on previous studies on former gold mines in the area, it is believed that early mafic intrusion suite appears to have contributed to the early hydrothermal enrichment of gold deposits through the action of water-rock, together with atmospheric precipitation and stratigraphic water. Due to favorable structural conditions during the Indosinian tectonic period, the late basic rock not only extracted metallogenic materials from the stratum but also acted as an important heat source for the metallogenic fluid circulation and mineralization, together with superposed mineralization of frequent tectonic activities on early deposits, finally forming into ore deposits in favorable structures. Therefore, we believe that the mafic intrusion suite in the late period of the region are closely related to the gold mineralization in the region, and it can be used as a prospecting mark for gold deposits in the area.},
     year = {2020}
    }
    

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  • TY  - JOUR
    T1  - Geochronology of Two Mafic Intrusions in Funing, Yunnan: Implications for Its Relationships with Carlin-like Gold Mineralization
    AU  - Pi Qiaohui
    AU  - Wei Chaowen
    AU  - Yu Huidong
    AU  - Lu Di
    Y1  - 2020/04/08
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    N1  - https://doi.org/10.11648/j.ijmpem.20200501.12
    DO  - 10.11648/j.ijmpem.20200501.12
    T2  - International Journal of Mineral Processing and Extractive Metallurgy
    JF  - International Journal of Mineral Processing and Extractive Metallurgy
    JO  - International Journal of Mineral Processing and Extractive Metallurgy
    SP  - 7
    EP  - 19
    PB  - Science Publishing Group
    SN  - 2575-1859
    UR  - https://doi.org/10.11648/j.ijmpem.20200501.12
    AB  - The relationship between mafic intrusion and gold deposits has always received substantial attention. Based on the petrography, mineralogy, and chronology of two mafic intrusion suites exposed in the Funing area, we found that the mafic intrusion suites have closely relationship with gold mineralization. The 255±4.9-Ma U-Pb age of the early mafic intrusion suite is much older than the 218.9±6.4-Ma (MSWD=1.2) U-Pb age of the late mafic intrusion suite. Based on previous studies on former gold mines in the area, it is believed that early mafic intrusion suite appears to have contributed to the early hydrothermal enrichment of gold deposits through the action of water-rock, together with atmospheric precipitation and stratigraphic water. Due to favorable structural conditions during the Indosinian tectonic period, the late basic rock not only extracted metallogenic materials from the stratum but also acted as an important heat source for the metallogenic fluid circulation and mineralization, together with superposed mineralization of frequent tectonic activities on early deposits, finally forming into ore deposits in favorable structures. Therefore, we believe that the mafic intrusion suite in the late period of the region are closely related to the gold mineralization in the region, and it can be used as a prospecting mark for gold deposits in the area.
    VL  - 5
    IS  - 1
    ER  - 

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Author Information
  • Earth Sciences Institute, Guilin University of Technology, Guilin, China

  • Earth Sciences Institute, Guilin University of Technology, Guilin, China

  • Earth Sciences Institute, Guilin University of Technology, Guilin, China

  • Earth Sciences Institute, Guilin University of Technology, Guilin, China

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