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Second -Derivate of MT Apparent Resistivity Data : A Possible Solution to Detectability

机译:MT表观电阻率数据的二阶导数:可检测性的可能解决方案

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Very broad band of natural magneto telluric (MT) signal with signal penetration determined by theskin depth provides MT method capability to probe shallow and deep features equally well albeitwith decreasing resolution as the depth increases. We used a new processing scheme involvingsecond derivative of the apparent resistivity curve to enhance the effects of thin conducting layersin continental crusts at different depth which are otherwise masked in conventional resistivitypseudo sections. As the second derivative of apparent resistivity curve exhibits a peak/ trough foreach interface, the configuration of an interface can be easily marked in a seismic-like plot ofthese data. Analyses of synthetic data over two different models, viz., Deccan Trap, India andRhine Graben-Black forest region, Germany demonstrate the potential of the scheme developed.
机译:极宽的自然磁碲信号(MT)信号具有由皮肤深度确定的信号穿透能力,尽管随着深度的增加分辨率降低,但MT方法能够很好地探测浅层和深层特征。我们使用了一种涉及表观电阻率曲线的二阶导数的新处理方案,以增强不同深度的大陆壳中薄导电层的作用,而在传统的电阻率伪剖面中,这些薄层被掩盖了。由于视电阻率曲线的二阶导数在每个界面上都显示出峰/谷,因此可以在这些数据的类似地震的图中轻松地标出界面的配置。对印度Deccan Trap和德国Rhine Graben-Black Forest地区这两种不同模型的综合数据进行的分析证明了该方案的潜力。

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