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LAS: A combination of the analytic signal amplitude and the generalised logistic function as a novel edge enhancement of magnetic data

机译:LAS:分析信号幅度和广义逻辑函数的组合作为磁数据的新颖边缘增强

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In the evaluation of magnetic field data, edge enhancement and detection techniques are important treatments for the interpretation of geological structures. In general geological sense, contiguity of deep and shallow magnetic sources leads to weak and intense anomalies that complicates the interpretation to disclose adjacent anomalous sources. Many of the existing filters for edge detection in magnetics mostly have the disadvantage that they require a reduction to pole transformation as the pre-process of the data or they cannot balance weak and intense anomalies and therefore fail in detecting edges of deep and shallow sources simultaneously. This study presents an improved edge detection filter LAS (logistic function of the analytical signal), based on the generalised logistic function configured by the ratio of derivatives of the analytical signal. This novel approach has the capability of reducing the dependence on the direction of the magnetization and also balancing anomalies of sources at different levels of depth. The feasibility of the method is examined on both theoretical and real data cases comparatively with some other methods that utilize the analytical signal in their basis. In comparison, the results demonstrate that the LAS method provides more accurate estimation of edge localization.
机译:在磁场数据的评估中,边缘增强和检测技术是用于地质结构解释的重要处理。在一般地质意义上,深层和浅磁性源的邻接导致弱和强烈的异常,使解释揭示相邻的异常来源。用于在磁性中的边缘检测的许多现有过滤器主要具有缺点,即它们需要将磁极转换减少作为数据的预处理,或者它们不能平衡弱和强烈的异常,因此在同时检测深度和浅源的边缘失败。本研究基于由分析信号的衍生物比率配置的广义逻辑函数,提出了改进的边缘检测滤波器LAS(分析信号的逻辑功能)。这种新颖的方法具有降低对磁化方向的依赖性以及在不同深度水平的源的平衡异常。在理论和实际数据情况下,对该方法的可行性相对较好地在其基础上使用分析信号的其他方法进行了相对的。相比之下,结果表明LAS方法提供更准确的边缘定位估计。

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