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胶西北石墨矿覆盖区金矿综合物探找矿方法和应用效果

Comprehensive geophysical exploration methods and application effects for gold deposits in the graphite covered area of Northwest Jiaodong

  • 摘要:
    研究目的 招平成矿带是胶西北地区重要的导矿构造,成矿地质条件优越。在招平成矿带南墅地区,金矿床隐伏在石墨矿之下,由于石墨矿具有极低的电阻率性质,屏蔽了一些电磁法的电磁信号向下穿透,致使电磁信号止于石墨矿部位,无法探测隐伏于石墨矿下的金矿床。为了厘清南墅地区金矿床的深部赋存及成矿特征,更好地指导该区下一步金矿找矿方向,需精选有效可行的物探勘探方法。
    研究方法 利用常规重磁电法及新技术广域电磁法、地微动天然源面波法、频谱激电法等综合物探找矿方法对石墨矿极低阻屏蔽区深部金矿进行综合分析研究。
    研究结果 优选了石墨矿覆盖区金矿综合物探精细找矿方法,确定了多源数据融合视角下招平成矿带的平面及深部空间展布特征,圈定出金矿激电异常位置。
    结论 通过钻探揭露剖析,验证了所推断金激电异常位置的准确性,实现了极低阻屏蔽区深部找矿新突破。

     

    Abstract:
    Objective Zhaoping metallogenic belt is an important ore conducting structure in the northwestern region of Jiaodong, with superior geological conditions for mineralization. In the Nanshu area of the Zhaoping metallogenic belt, gold deposits are hidden beneath graphite deposits. Due to the extremely low electrical resistivity of graphite deposits, some electromagnetic signals from electromagnetic methods are shielded from penetrating downwards, resulting in electromagnetic signals stopping at the graphite deposit site and making it impossible to detect gold deposits hidden beneath graphite deposits.In order to clarify the deep occurrence and mineralization characteristics of the gold deposits in Nanshu area and better guide the next step of gold exploration in the area, feasible and effective geophysical exploration methods need to be selected.
    Methods This article aims to comprehensively analyze and study deep gold deposits in graphite ore extremely low resistance shielding areas through the use of conventional gravity magnetic method and new technologies such as wide area electromagnetic method, microseismic natural source surface wave method, and spectral induced polarization method.
    Results A comprehensive geophysical fine prospecting method for gold deposits in graphite ore−covered areas was optimized.The planar and deep spatial distribution characteristics of the Zhaoping metallogenic belt from the perspective of multi−source data fusion were determined, and the locations of induced polarization anomalies for gold deposits were delineated.
    Conclusions Through drilling and analysis, the accuracy of the inferred location of the gold induced polarization anomaly has been verified, achieving a new breakthrough in deep mineral exploration in extremely low resistance shielding areas.

     

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