摘要
多尺度分析方法可以在不同的尺度上将信号分解成为轮廓和细节,这样有助于对信号进行更为精细的处理。简要介绍了多尺度方法应用于重磁数据处理的基本思想,从理论上讨论了基于多尺度方法提高重磁场深/浅源异常对比度的方法,并对其作了严格的证明。理论分析及模型实例表明,多尺度方法虽然不能将性质相同的异常完全分离,但可以有效地提高深源异常对浅源异常的对比度。在有浅源异常干扰的地区,可以有效地压制浅部干扰,突出深部场源信息。
A multiscale method can decompound the signal into outline and detail parts,which is helpfull greatly to a finer analysis.A brief introduction into the conception to apply the method in gravity data processing and the theory to improve the contrast of deep/shallow source anomaly are presented and proved strictly. Theoretical analysis and numerical modeling results show that the multiscale method does enhance the contrast of deep/shallow source anomaly though it can not completely separate the anomaly.This method can suppress disturbance from shallow source and enhance the information from deep source.
出处
《江汉石油学院学报》
CSCD
北大核心
1998年第2期48-51,共4页
Journal of Jianghan Petroleum Institute
关键词
重力勘探
位场源
对比度
多尺度分析
gravity data processing
potential field
(multiscale analysis)
correlation