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A multiple parameter extraction and electromagnetic coupling correction technique for time domain induced polarisation full waveform data

机译:时域感应极化全波形数据的多参数提取和电磁耦合校正技术

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摘要

The time domain induced polarisation (TDIP) method is characterised by a simple explanation and operational approach, and is used widely to prospect for various metal sulfide deposits. However, the existing TDIP method is parameterised with fewer interpretive output attributes than the frequency domain induced polarisation (FDIP) method, and there has been far less emphasis on electromagnetic (EM) coupling in the TDIP method. A new and simple method has been devised for the extraction of multiple parameters and the suppression of EM-coupling responses in full waveform TDIP data. The essence of this approach is the transformation of the TDIP rectangular wave into the fundamental wave and a series of odd harmonics using a discrete Fourier transform. By using real and imaginary components of the fundamental and odd harmonics, we can calculate various FDIP parameters, including the per cent frequency effect (PFE) and the phase. The decoupled PFE coefficients and decoupled phases can then be used to remove the EM-coupling response. This new method has been applied to a data set collected near a poly-metallic mine in the Tibetan Plateau. A comparison between the TDIP and FDIP methods with central gradient arrays was performed. The results indicate that the TDIP apparent chargeability results are affected greatly by the EM-coupling response. The PFEs and phases extracted from the TDIP full waveform data are in good agreement with those obtained from the FDIP data. Moreover, the locations of the high decoupled PFE coefficients and the large negative decoupled phases are consistent with the locations of known ore veins. This method can provide additional parameters for the subsurface media, improve the practical application effect and enrich the functionality of TDIP methods.
机译:时域感应极化(TDIP)方法具有简单的解释和操作方法的特点,被广泛用于各种金属硫化物矿床的勘探。但是,与频域感应极化(FDIP)方法相比,现有TDIP方法的参数化解释性输出属性较少,并且TDIP方法中对电磁(EM)耦合的重视程度大大降低。已经设计出一种新的简单方法来提取多个参数并抑制全波形TDIP数据中的EM耦合响应。这种方法的本质是使用离散傅立叶变换将TDIP矩形波转换为基波和一系列奇次谐波。通过使用基波和奇次谐波的实部和虚部,我们可以计算各种FDIP参数,包括百分比频率效应(PFE)和相位。然后可以使用解耦的PFE系数和解耦的相位来消除EM耦合响应。该新方法已应用于青藏高原多金属矿附近收集的数据集。使用中央梯度阵列对TDIP和FDIP方法进行了比较。结果表明,TDIP的表观充电性结果受EM耦合响应的影响很大。从TDIP全波形数据中提取的PFE和相位与从FDIP数据获得的PFE和相位非常一致。此外,高解耦PFE系数和大负解耦相的位置与已知矿脉的位置一致。该方法可以为地下介质提供附加参数,提高实际应用效果,丰富TDIP方法的功能。

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  • 来源
    《Exploration Geophysics》 |2019年第2期|113-123|共11页
  • 作者单位

    China Univ Geosci, Sch Geophys & Informat Technol, Beijing, Peoples R China|Chinese Acad Geol Sci, Inst Geophys & Geochem Explorat, Res Lab Electromagnet Detect Technol, Langfang, Peoples R China;

    Chinese Acad Geol Sci, Inst Geophys & Geochem Explorat, Res Lab Electromagnet Detect Technol, Langfang, Peoples R China;

    China Univ Geosci, Sch Geophys & Informat Technol, Beijing, Peoples R China|China Aero Geophys Survey & Remote Sensing Ctr La, Informat Period Dept, Beijing, Peoples R China;

    Chinese Acad Geol Sci, Inst Geophys & Geochem Explorat, Res Lab Electromagnet Detect Technol, Langfang, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    induced polarisation; time domain; frequency domain; electromagnetic-coupling correction; full waveform data;

    机译:诱导极化;时域;频域;电磁耦合校正;全波形数据;

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