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Potential field gradient modulus maxima edge detection based on wavelet transform

机译:基于小波变换的潜在场梯度模量Maxima边缘检测

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As the Fourier transform only can confirm the overall nature of the signal singularity, especially in analyzing the geological body edges (for instance, the deep faults) for the upward extended signal, the detected edges from the horizontal total gradient modulus that based on the Fourier transform are often blurred and smooth, so it is difficulties to confirm the details of the edges. The wavelet transform is with the good time-frequency localization, and its coefficient gradient maxima are very sensitive to the signal singular, which can be used to analyze the signal singular points location and singularity degree. We proposed a potential field gradient modulus maxima edge detection method that based on wavelet transform, which utilizes the horizontal gradient variation of the wavelet transform coefficient to synthesize the wavelet gradient modulus, and with the modulus maxima to perform the edges detection. The theoretical model tests and the practical fault analysis for the Middle-Lower Reach of Yangtze River indicates the outcomes with proposed method is of higher resolution as well as stronger anti-jamming capability than those from the horizontal total gradient modulus and its maxima that based on the Fourier transform.
机译:由于傅里叶变换只能确认信号奇异性的整体性质,特别是在分析向上扩展信号的地质体边缘(例如,深度故障)时,检测到的来自傅立叶的水平总梯度模量的检测到边缘变换往往模糊而平滑,因此确认边缘的细节是困难的。小波变换具有良好的时频定位,其系数梯度最大值对信号奇异非常敏感,可用于分析信号奇异点位置和奇异度。我们提出了一种基于小波变换的潜在场梯度模量Maxima边缘检测方法,其利用小波变换系数的水平梯度变化来合成小波梯度模量,以及模量最大值执行边缘检测。长江中下游的理论模型试验和实际故障分析表明了采用较高分辨率的方法以及比水平总梯度模量及其最大值的抗干扰能力更高的抗干扰能力傅里叶变换。

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