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2-D time-frequency inversion of 1-D geo-electrical models for transient electromagnetic method

机译:瞬态电磁法1-D地球电模型的2-D时间频率

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The pure secondary field features of transient electromagnetic (TEM) method have its observed data have similar shapes for different geo-electrical models so that 1-D fitting inversion results in time-domain are not as good as results in frequency-domain. In this paper, developing 1-D time-domain signals to 2-D time-frequency (T-F) plane and using minimum structure inversion algorithm, we realize joint T-F inversion. It is shown that T-F inversion is provided with higher adaptability and the inversion results are much improved by means of it.
机译:瞬态电磁(TEM)方法的纯次级场特征具有其观察到的数据对于不同的地质电模型具有相似的形状,使得1-D拟合反演导致时域的结果与频域中的结果不如频域。本文将1-D时域信号开发到2-D时间频率(T-F)平面并使用最小结构反转算法,实现关节T-F反转。结果表明,通过较高的适应性提供T-F反转,并且通过它的转换结果很大。

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