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Basic Geological and Geochemical Analysis in Wenquanbingzhan Area

Received: May 13, 2019    Accepted: Jun. 25, 2019    Published: Jul. 18, 2019
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Abstract

According to the basic geology study, the feature of the element association and the analysis on characteristic element abnormal combination, we think that there are large scale intermediate-basic volcanic (subvolcanic) rocks with some medium acid intruded rocks or vein rocks groups by the work of 1 to 50000 scale geochemical exploration in the north Sanjiang-Wenquanbingzhan area. The fractures of Yanshiping and Wenquanbingzhan area etc. are the big fractures of guide rock and rock-controlled and the fracture zones in the northwest of Chuduo-Chaqiong play an ore conducting and controlling role in the process. The metallogenic condition of anticline structure is better than that of syncline structure. Based on the above consideration, the diagenesis and mineralization in this area are closely related to the intermediate-basic and acidic magmas activity. Copper and polymetallic ores can be classified to volcanics-type and sedimentary-reformed type.

DOI 10.11648/j.earth.20190804.11
Published in Earth Sciences ( Volume 8, Issue 4, August 2019 )
Page(s) 217-227
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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), 2024. Published by Science Publishing Group

Keywords

Wenquanbingzhan Study Area, Metallogenic Condition, Geochemical Analysis, Factor Metering, Medium Acid Volcanic Rocks, Metallogenic Structure

References
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  • APA Style

    Zheng Xiang Guang, Lu Lin, Mao Yi Feng, Wang Chen, Meng Jun Feng. (2019). Basic Geological and Geochemical Analysis in Wenquanbingzhan Area. Earth Sciences, 8(4), 217-227. https://doi.org/10.11648/j.earth.20190804.11

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    ACS Style

    Zheng Xiang Guang; Lu Lin; Mao Yi Feng; Wang Chen; Meng Jun Feng. Basic Geological and Geochemical Analysis in Wenquanbingzhan Area. Earth Sci. 2019, 8(4), 217-227. doi: 10.11648/j.earth.20190804.11

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    AMA Style

    Zheng Xiang Guang, Lu Lin, Mao Yi Feng, Wang Chen, Meng Jun Feng. Basic Geological and Geochemical Analysis in Wenquanbingzhan Area. Earth Sci. 2019;8(4):217-227. doi: 10.11648/j.earth.20190804.11

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  • @article{10.11648/j.earth.20190804.11,
      author = {Zheng Xiang Guang and Lu Lin and Mao Yi Feng and Wang Chen and Meng Jun Feng},
      title = {Basic Geological and Geochemical Analysis in Wenquanbingzhan Area},
      journal = {Earth Sciences},
      volume = {8},
      number = {4},
      pages = {217-227},
      doi = {10.11648/j.earth.20190804.11},
      url = {https://doi.org/10.11648/j.earth.20190804.11},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.earth.20190804.11},
      abstract = {According to the basic geology study, the feature of the element association and the analysis on characteristic element abnormal combination, we think that there are large scale intermediate-basic volcanic (subvolcanic) rocks with some medium acid intruded rocks or vein rocks groups by the work of 1 to 50000 scale geochemical exploration in the north Sanjiang-Wenquanbingzhan area. The fractures of Yanshiping and Wenquanbingzhan area etc. are the big fractures of guide rock and rock-controlled and the fracture zones in the northwest of Chuduo-Chaqiong play an ore conducting and controlling role in the process. The metallogenic condition of anticline structure is better than that of syncline structure. Based on the above consideration, the diagenesis and mineralization in this area are closely related to the intermediate-basic and acidic magmas activity. Copper and polymetallic ores can be classified to volcanics-type and sedimentary-reformed type.},
     year = {2019}
    }
    

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  • TY  - JOUR
    T1  - Basic Geological and Geochemical Analysis in Wenquanbingzhan Area
    AU  - Zheng Xiang Guang
    AU  - Lu Lin
    AU  - Mao Yi Feng
    AU  - Wang Chen
    AU  - Meng Jun Feng
    Y1  - 2019/07/18
    PY  - 2019
    N1  - https://doi.org/10.11648/j.earth.20190804.11
    DO  - 10.11648/j.earth.20190804.11
    T2  - Earth Sciences
    JF  - Earth Sciences
    JO  - Earth Sciences
    SP  - 217
    EP  - 227
    PB  - Science Publishing Group
    SN  - 2328-5982
    UR  - https://doi.org/10.11648/j.earth.20190804.11
    AB  - According to the basic geology study, the feature of the element association and the analysis on characteristic element abnormal combination, we think that there are large scale intermediate-basic volcanic (subvolcanic) rocks with some medium acid intruded rocks or vein rocks groups by the work of 1 to 50000 scale geochemical exploration in the north Sanjiang-Wenquanbingzhan area. The fractures of Yanshiping and Wenquanbingzhan area etc. are the big fractures of guide rock and rock-controlled and the fracture zones in the northwest of Chuduo-Chaqiong play an ore conducting and controlling role in the process. The metallogenic condition of anticline structure is better than that of syncline structure. Based on the above consideration, the diagenesis and mineralization in this area are closely related to the intermediate-basic and acidic magmas activity. Copper and polymetallic ores can be classified to volcanics-type and sedimentary-reformed type.
    VL  - 8
    IS  - 4
    ER  - 

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Author Information
  • The Second Comprehensive Geophysical Survey Team Company, Shaanxi Bureau of Geology and Mineral Resources, Xi’an, China

  • The Second Comprehensive Geophysical Survey Team Company, Shaanxi Bureau of Geology and Mineral Resources, Xi’an, China

  • The Second Comprehensive Geophysical Survey Team Company, Shaanxi Bureau of Geology and Mineral Resources, Xi’an, China

  • The Second Comprehensive Geophysical Survey Team Company, Shaanxi Bureau of Geology and Mineral Resources, Xi’an, China

  • The Second Comprehensive Geophysical Survey Team Company, Shaanxi Bureau of Geology and Mineral Resources, Xi’an, China

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