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    中国百强科技报刊

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    Volume 47 Issue 10
    Oct.  2022
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    Article Contents
    Zheng Yi, 2022. Large-Scaled Structure-Alteration-Mineralization Mapping of the Hydrothermal Deposits: Basic Principle and Precautions. Earth Science, 47(10): 3603-3615. doi: 10.3799/dqkx.2022.295
    Citation: Zheng Yi, 2022. Large-Scaled Structure-Alteration-Mineralization Mapping of the Hydrothermal Deposits: Basic Principle and Precautions. Earth Science, 47(10): 3603-3615. doi: 10.3799/dqkx.2022.295

    Large-Scaled Structure-Alteration-Mineralization Mapping of the Hydrothermal Deposits: Basic Principle and Precautions

    doi: 10.3799/dqkx.2022.295
    • Received Date: 2022-06-30
    • Publish Date: 2022-10-25
    • Large-scale mapping of the hydrothermal deposits refers to the geological mapping with the scales of 1∶1 000 and the larger scales, which is mainly used to record various geological phenomena that can be directly observed with the naked eye, such as outcrops, flat tunnels, boreholes and hand specimens in the mining area. The purpose of large-scale mapping is to identify the metallogenic characteristics, spatial distribution and temporal evolution of the hydrothermal deposits, which are useful for accurately constraining the genetic type and metallogenic process of hydrothermal deposits, as well as assisting further prospecting and exploration. In the field survey, the beginners do not know how to describe and record the complex phenomena of the hydrothermal deposits, and they are also not very clear about what to fill and how to map. To address these issues, we try to weaken the genetic type of the ore deposit from the basic principle, focusing on the formation process of the structure, fluid, alteration and mineralization of the hydrothermal deposit, and propose "ore-forming fluid + fresh wall rock → wall rock alteration + ore" as a universal formula for the formation of hydrothermal deposits, and puts forward the analogies of "structure → skeleton" and "alteration → flesh". In addition, we focus on some long-ignored aspects in the process of large-scale mapping of hydrothermal deposits, such as identification of metallogenic environment, ore-forming fluid channels and traps, hydrothermal filling and metasomatism, and identification of vein cross-cutting, etc. Furthermore, we eventual focus is on explaining the hidden genetic inspiration behind these geological phenomena.

       

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