三维断层模型的MT倾子响应数值模拟

    Numerical simulation of MT tipper response based on 3D fault models

    • 摘要: 倾子矢量作为大地电磁测深法中的一个重要参数,适用于推断介质横向不均匀的断裂构造。地下断层构造一般具有三维性和复杂性的特点,为了揭示三维断层模型的大地电磁倾子响应特征,本文基于矢量有限元法开展了三维断层模型的大地电磁倾子响应数值模拟。首先,通过理论模型试算,并与前人的有限元法计算结果对比,验证了三维倾子正演计算程序的正确性。在此基础上,分别对直立断层、正断层、逆断层和走滑断层4种典型的三维断层模型进行正演模拟,获得倾子响应的实部、虚部、振幅和相位。模拟结果表明:在两种极化模式下,倾子实部、虚部和振幅响应特征对4种不同类型断层的性质、走向、倾向等信息反映效果明显,同时又表现了断层横向不均匀的边界位置,可作为判别断层类型和特征的重要依据;相比于倾子实部、虚部和振幅的响应特征,倾子相位响应特征较为复杂,难以有效反映断层特征信息。

       

      Abstract: The tipper vector,a significant parameter in magnetotelluric(MT) sounding,is applicable to infer fault structures that cause lateral inhomogeneity of media.Subsurface faults typically exhibit three-dimensionality and complexity.To reveal the MT tipper response characteristics in 3D fault models,this study conducted numerical simulations of the MT tipper response in 3D fault models based on the vector finite element method.First,the validity of the 3D tipper forward modeling program was verified through theoretical model calculations and comparisons with previous finite element results.Subsequently,four typical 3D models for vertical,normal,reverse,and strike-slip faults were employed for forward modeling,obtaining the response characteristics of the real part,imaginary part,amplitude,and phase of the tipper.The simulation results are as follows:(1) In two polarization modes,the response characteristics of the real part,imaginary part,and amplitude of the tipper effectively reflect the properties,strikes,and dip directions of the four different faults while indicating the location of the laterally inhomogeneous boundaries,thus serving as a significant basis for discriminating fault types and characteristics;(2)In contrast,the relatively complex response characteristics of the phase fail to effectively mirror the fault characteristics.

       

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