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A new efficient method for topographic distortion correction, analytical continuation, vertical derivatives and using equivalent source technique: Application to field data

机译:一种新的有效的地形畸变校正,分析连续,垂直导数和使用等效源技术的方法:应用于现场数据

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In general, potential field data are noisy due to the surveys in rugged topography. Standard reduction techniques are not fully adequate to eliminate this problem. Most of the interpretation techniques require the observations measured on the horizontal surface. Furthermore, upward and downward continuations, and vertical derivatives can improve the ambiguity in the potential field data. In present, there are methods for the application of the analytical continuations and derivatives, but these are not successful enough due to technical restrictions and unwanted edge effects. In this paper, an easy and efficient technique known as the equivalent source is applied to the observations made over the rugged topography. The presented method is tested on synthetic example using an anomaly of a sphere located below the synthetic topography. At first, our method is applied only to obtain a topographic distortion corrected map by moving forward windowed parts of the area. Afterwards, analytic continuations of the topographic distortion corrected map are obtained. Finally, a vertical derivative map is obtained from the analytic continuations of the topographic distortion corrected map. Amplitudes are controlled along profiles on top of theoretical and calculated spheres. A good correlation can be observed from the amplitude values. This method is also applied to the field data. The second vertical derivative map is produced from the topographic distortion corrected and 5 km upward continued gravity map of the region. We note that by the interpretations identified faults in these map are in good agreement with the faults shown in the structural map of the region.
机译:通常,由于崎top地形的调查,潜在的现场数据比较嘈杂。标准减少技术不足以消除此问题。大多数解释技术都需要在水平表面上进行观测。此外,向上和向下的连续性以及垂直导数可以改善潜在场数据中的歧义。当前,存在应用分析连续体和导数的方法,但是由于技术限制和不希望的边缘效应,这些方法还不够成功。在本文中,将一种简单有效的技术(称为等效源)应用于在崎top地形上进行的观测。在合成示例上使用位于合成地形下面的球体异常测试了所提出的方法。首先,我们的方法仅适用于通过向前移动区域的加窗部分来获得地形失真校正的地图。之后,获得了地形畸变校正图的解析连续性。最后,从地形畸变校正图的解析连续性获得垂直导数图。沿理论球和计算球顶部的轮廓控制振幅。从振幅值可以观察到良好的相关性。该方法也适用于现场数据。根据校正的地形畸变和该区域向上5 km的连续重力图生成第二个垂直导数图。我们注意到,通过解释,这些地图中确定的断层与该区域的结构图中所示的断层非常吻合。

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