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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Composite continuous wavelet transform of potential fields with different choices of analyzing wavelets
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Composite continuous wavelet transform of potential fields with different choices of analyzing wavelets

机译:不同分析小波选择的势场复合连续小波变换

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In potential field problems, the continuous wavelet transform (CWT) has allowed the estimation of the source properties, such as the depth to the source and the structural index (N). The natural choice for the analyzing wavelets has been the set belonging to the Poisson kernel. However, a much larger set of analyzing wavelets has been used for analyzing signals other than potential fields. Here we extend the CWT of potential fields to other wavelet families. Since the field is intrinsically dilated with Poissonian wavelets from the source depth to the measurement level, distortions are unavoidably introduced when CWT uses a different wavelet from the measurement level to other scales. To fix the problem, we define a new form for the continuous wavelet transform convolution product, called “composite continuous wavelet transform” (CCWT). CCWT removes the field dilations with Poisson wavelets, intrinsically contained at the measurement level and replaces them with dilations performed with any other kind of wavelet. The method is applied to synthetic and real cases, involving sources as poles, dipoles, intrusions in complex magnetized basement topography and buried steel drums, from measurements taken at the Stanford University test site. CCWT takes advantage from the special features of the several considered wavelets, e.g., the Gaussian wavelet is useful for its low pass filtering characteristic and Morlet wavelet for its localization property. Hence, depending on the case, an important parameter for the choice of the analyzing wavelet is its central frequency.
机译:在潜在的现场问题中,连续小波变换(CWT)允许估算源属性,例如到源的深度和结构索引(N)。分析小波的自然选择是属于泊松核的集合。但是,除了势场以外,还使用了更多的分析小波集来分析信号。在这里,我们将势场的CWT扩展到其他小波族。由于该场本质上是用泊松小波从源深度扩展到测量水平的,因此当CWT使用从测量水平到其他比例的不同小波时,不可避免地会引入失真。为了解决该问题,我们为连续小波变换卷积积定义了一种新形式,称为“复合连续小波变换”(CCWT)。 CCWT去除了包含在测量级别上的泊松子波的场膨胀,并用其他任何种类的子波进行的膨胀代替了它们。该方法适用于合成案例和实际案例,这些资源来自极地,偶极子,复杂的磁化地下室地形中的侵入物以及埋在地下的钢桶中,这些都是根据斯坦福大学测试现场进行的测量得出的。 CCWT利用了几个考虑的子波的特殊功能,例如,高斯子波因其低通滤波特性而有用,而Morlet小波因其定位特性而有用。因此,根据情况,选择分析小波的重要参数是其中心频率。

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