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首页> 外文期刊>Journal of Applied Geophysics >A fast interpretation method of gravity gradiometry data based on magnetic dipole localization
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A fast interpretation method of gravity gradiometry data based on magnetic dipole localization

机译:基于磁偶极定位的重力梯度数据快速解释方法

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In this paper, we proposed a fast interpretation method for gravity gradiometry data, based on the magnetic dipole localization method. It could automatically and rapidly locate the horizontal and vertical positions of gravity targets without prior information. This method was successfully tested on synthetic data. Compared with gradient ratio method (tilt-depth) and Euler deconvolution, our method provided good performance in the gravity gradiometry data with high noise levels and superimposed fields. Point selection was processed among the inversion results to improve the resolution of our method. Statistical analysis and Gaussian fitting were also used to improve the stability and accuracy of the calculation. Finally, we applied this algorithm to gravity gradiometry data over Vinton Dome; the results are consistent with previous research in this area. (C) 2017 Published by Elsevier B.V.
机译:本文基于磁偶极局部化方法提出了一种快速解释方法,用于重力梯度计数数据。 没有先前信息,它可以自动且快速地定位重力目标的水平和垂直位置。 该方法在合成数据上成功测试。 与梯度比法(倾斜深度)和欧拉去折叠相比,我们的方法在具有高噪声水平和叠加的领域的重力梯度数据中提供了良好的性能。 点选择是在反演结果中处理的,以改善方法的解决方案。 统计分析和高斯配件也用于提高计算的稳定性和准确性。 最后,我们将该算法应用于Vinton Dome的重力梯度数据; 结果与此领域的先前研究一致。 (c)2017年由Elsevier B.V发布。

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