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    九万大山地区断裂构造分形特征及其地质意义

    Fractal characteristics of fractures in Jiuwandashan area and their geological significance

    • 摘要: 提要:本文借助于陆地卫星多波段卫星遥感影像,对九万大山区断裂构造进行了综合解译,结合区域地质背景,基于分形几何学的理论基础,对遥感解译断裂构造进行了定量化研究。结果显示,九万大山区断裂构造的分维值较高,显示断裂带结构复杂、构造活动强烈;元宝山子区断裂构造分维值明显偏低,其中北东向断裂构造的分维值大于北西向断裂构造的分维值,说明区内以北东向断裂构造为主,属主导性断裂构造,这恰好与区域构造特征相吻合。

       

      Abstract: Abstract:The fractal structure of the fracture makes it possible to give a quantitative description. The fractal dimension value of the fracture can indicate the deposit location and the migration of ore-forming fluids. The high fractal dimension value can suggest the intense tectonic movement favorable for the activation of elements, the migration and concentration of ore-forming fluids, and the formation of large and super-large ore deposits. By means of multi-band remote sensing images in combination with the regional geological background, the author interpreted the fractures and made a quantitative investigation based on the theory of fractal geometry. The results show that there exists a high fractal dimension value of fracture in Jiuwandashan area, which shows the complicated fracture belt and the intense tectonic movement. Nevertheless, the fractal dimension value of fracture is relatively low in Yuanbaoshan area. In addition, the fractal dimension value of the northeast fracture is higher than that of the northwest fracture, suggesting the dominating property of the northeast fracture in this area, which is consistent with the regional tectonic characteristics.

       

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