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Regional Crust Density Analysis Based on Multi-Scale Wavelet of Empirical Orthogonal Gravity Inversion

机译:基于经验正交重力反演的多尺度小波分析的区域地壳密度

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To further improve the performance of regional crust density analysis algorithm and the accuracy of the abnormal regional forecast, this Thesis puts forward a kind of regional crust density analysis based on multi-scale wavelet of empirical orthogonal gravity inversion. Firstly, it makes use of gravity inversion process to obtain the eigenvector of abnormal region in the gravity field within the study region and obtain the principal component of time series of gravity inversion data through the empirical orthogonal method; secondly, it conducts more carefully information processing and extraction for the principal component of time series with multi-scale wavelet to obtain more precise forecasted position of the abnormal region; finally, the experimental comparison of the regional crust density analysis did somewhere in the Northeast shows that the proposed algorithm has higher accuracy of the abnormal position forecast of crust density and that the calculation complexity does not increase significantly.
机译:为了进一步提高区域地壳密度分析算法的性能和异常区域预报的准确性,提出了一种基于经验正交重力反演的多尺度小波分析的区域地壳密度分析方法。首先,利用重力反演过程,获得经验区域内重力场异常区域的特征向量,并通过经验正交方法获得重力反演数据时间序列的主分量。其次,利用多尺度小波对时间序列的主成分进行更仔细的信息处理和提取,以得到更准确的异常区域预测位置。最后,通过对东北地区某区域地壳密度分析的实验比较,表明该算法对地壳密度异常位置预测具有较高的精度,且计算复杂度不会明显增加。

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