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Source Edge Detection of Potential Field Data Using Wavelet Decomposition

机译:使用小波分解的潜在场数据的源边缘检测

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摘要

Edge detection of the sources of potential field anomaly is an important step in the interpretation of subsurface source geometries. The conventional methods based on calculation of horizontal or vertical derivatives identify the edges or center of sources by minima, maxima, or zero values in the transformed data. We present a wavelet source edge detector method (WSED) using wavelet multiresolution analysis to identify potential field sources boundaries. The two-dimensional wavelet decomposition is an effective method to understand the frequency components of the signal in different directions. We use a 2D-discrete wavelet transform using Haar wavelets in resolving lateral edges for source edge detection. We test the method on synthetic magnetic anomalies due to sources of complex geometries generated using prismatic sources. We investigated the robustness of the method on the magnetic data of the Bishop model and found the results useful in resolving the edges. We applied the method to gravity data of the north Delhi fold belt, India, to identify boundaries of different geological formations. Our results indicate distinct properties of the source edges in the wavelet domain, which is for the first time reported for the interpretation of the potential field anomalies.
机译:位场异常源的边缘检测是地下源几何解释的重要步骤。基于水平或垂直导数计算的传统方法通过变换数据中的最小值、最大值或零值来识别源的边缘或中心。提出了一种利用小波多分辨率分析识别潜在场源边界的小波源边缘检测方法。二维小波分解是理解信号在不同方向上的频率分量的有效方法。我们使用二维离散小波变换,使用Haar小波分解侧面边缘,用于源边缘检测。我们在合成磁异常上测试了该方法,该异常是由使用棱镜源生成的复杂几何形状的源引起的。我们研究了该方法对Bishop模型的磁数据的鲁棒性,发现其结果有助于解决边缘问题。我们将该方法应用于印度北德里褶皱带的重力数据,以确定不同地质构造的边界。我们的结果表明,震源边缘在小波域具有明显的特性,这是首次报道用于解释位场异常。

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