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自适应正则化滤波化极方法研究

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化极是消除磁力异常斜磁化影响的关键步骤,可以在波数域(频率域)和空间域中实现.相比于空间域,在波数域(频率域)进行化极简单且高效,但在低纬度地区存在不稳定性问题,因此明确低纬度地区的范围,研究稳定、实用、精度高的低纬度地区化极方法具有重要意义.本文通过理论研究得出化极因子振幅的最大值为2时,对应的磁化倾角的值为±45°,当磁化倾角在该范围内时,引起化极不稳定.因此采用正则化思想,提出了自适应正则化滤波化极方法(ARF-RTP),该方法利用化极因子振幅构建正则化滤波函数,并以振幅值等于2作为约束计算化极方法的参数值,从而实现自适应化极处理,提高了化极方法的稳定性及实用性.同时结合迭代算法提高了此方法的精度,有效地解决了低纬度地区化极的不稳定性问题.自适应正则化滤波这一思想不但可以解决化极的不稳定性问题,而且可以解决分量转换或者磁化方向转换的不稳定性问题以及类似数据处理中的不稳定性问题,具有广阔的推广应用前景.
Research on the adaptive regularization filtering method of reduction-to-the-pole
Reduction-to-the-pole(RTP)is a significant step in eliminating the effects of oblique magnetization on magnetic anomaly.This process can be conducted in both the wave-number(frequency domain)and the spatial domains.The RTP in the wave-number domain(frequency domain)is more efficient than in the spatial domain,but it can be unstable in low latitude areas.Thus,it is necessary to define the scope of the low latitude areas and develop stable,practical,and high-precision RTP methods.In this paper,the theoretical study shows that the maximum value of the amplitude is 2,and the corresponding magnetization inclination is±45°.Within this range of magnetization inclination,causing the instability in RTP procedure.To address this issue,an adaptive regularization filtering method of reduction-to-the-pole(ARF-RTP)is proposed based on the regularization idea.The method constructs a regularization filtering function using the amplitude of RTP factor,and with the amplitude value of 2 as the constraint,the determination value of the parameter in the method is calculated to realize the adaptive RTP of magnetic anomaly,which improves the stability and practicability of the method.Additionally,an iterative algorithm is used to improve the accuracy of the method.The proposed ARF-RTP method effectively solves the instability problem of the RTP in the low latitude areas.The accuracy,stability,and practicality of the method are verified using synthetic models and real data.The adaptive regularization filtering can not only solve the instability problem of RTP but also address instability problems in data processing,such as component transformation or magnetization direction transformation of magnetic field.The ARF-RTP method has broad application prospects.

Reduction-to-the-pole(RTP)Low latitudes areasAmplitudeAdaptive regularization filteringIterative algorithm

何涛、王皓、张义蜜、王万银、Colin G.Farquharson、J.Kim Welford

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长安大学地质工程与测绘学院,西安 710054

Department of Earth Sciences,Memorial University of Newfoundland,St.John's,AlB 3X5,Canada

海洋油气勘探国家工程研究中心,北京 100028

中国科学院海洋地质与环境重点实验室,山东青岛 266071

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化极 低纬度地区 振幅 自适应正则化滤波 迭代算法

国家重点研发计划中国海油科技项目海洋油气勘探国家工程研究中心开放基金(2022)

2017YFC0602202

2024

地球物理学报
中国地球物理学会 中国科学院地质与地球物理研究所

地球物理学报

CSTPCD北大核心
影响因子:3.703
ISSN:0001-5733
年,卷(期):2024.67(3)
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