基于多尺度边缘的重力异常分离方法
Separation of Gravity Anomalies Based on Multiscale Edges
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摘要: 利用多尺度边缘分析理论,对重力异常的小波多重分解法作了改进,提出了基于多尺度边缘的重力异常分离方法。实验表明,改进方法除保留了多重分解法的优点外,还能够同时实现异常的纵向和横向分离,而且可以根据每个场源对应的多尺度边缘的分布情况确定小波分解的阶数,有利于单一异常特征的提取。利用该方法对琉球俯冲带西南端区域的船测重力资料进行了处理分析,结果与该区域的地质构造具有很好的对应关系。Abstract: The wavelet approach for multiple decomposition of gravity anomalies is modified using multiscale edge analysis theory,and a separation method based on multiscale edges is proposed.The experimental results show that the new method has the same advantages of multiple decomposition method,and can be used to simultaneously perform vertical and lateral separation of anomalies.A proper degree for decomposition can be determined according to the distribution of multiscale edges of each source with respect to the scale,it is very useful to isolate single anomaly.Shipborne gravity data in southwest of Ryukyu subduction zone are analyzed.The result has good coherence with the geological tectonics in this area.