{"title":"Anisotropic Wave Separation Elastic Reverse Time Migration Based on the Pseudo-Decoupled Wave Equations in VTI Media","authors":"Yu Zhong;Qinghui Mao;Yangting Liu;Mei He;Kun Zou;Kai Xu;Hanming Gu;Zeyun Shi;Haibo Huang;Yuan Zhou","doi":"10.1109/LGRS.2024.3494763","DOIUrl":null,"url":null,"abstract":"Seismic exploration risk can be decreased by high-precision migration techniques. Imaging anisotropic multicomponent seismic data in areas with developed cracks and sedimentation is challenging. We introduce an efficient anisotropic wave separation elastic reverse time migration (RTM) to image anisotropic multicomponent seismic data in this letter. The elastic waves are decomposed into P- and S-waves for subsequent anisotropic wave separation elastic RTM (AWSERTM) to reduce crosstalk noise and improve imaging accuracy. In this new method, the pseudo-decoupled wave equations of transverse isotropic (TI) media with a vertical symmetry axis vertical transversely isotropic (VTI) are derived based on the decomposition of the anisotropic elastic stiffness parameters into anisotropic P- and S-wave stiffness parameters. Forward and backward anisotropic P- and S-waves can then be efficiently obtained by numerical solution of the pseudo-decoupled wave equations using the finite difference (FD) method. Combining the vector imaging condition, the high-quality AWSERTM’s results can be obtained. Synthetic examples from the modified HESS VTI model demonstrate the correctness and progressiveness of the proposed method.","PeriodicalId":91017,"journal":{"name":"IEEE geoscience and remote sensing letters : a publication of the IEEE Geoscience and Remote Sensing Society","volume":"21 ","pages":"1-5"},"PeriodicalIF":0.0000,"publicationDate":"2024-11-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"IEEE geoscience and remote sensing letters : a publication of the IEEE Geoscience and Remote Sensing Society","FirstCategoryId":"1085","ListUrlMain":"https://ieeexplore.ieee.org/document/10749969/","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Seismic exploration risk can be decreased by high-precision migration techniques. Imaging anisotropic multicomponent seismic data in areas with developed cracks and sedimentation is challenging. We introduce an efficient anisotropic wave separation elastic reverse time migration (RTM) to image anisotropic multicomponent seismic data in this letter. The elastic waves are decomposed into P- and S-waves for subsequent anisotropic wave separation elastic RTM (AWSERTM) to reduce crosstalk noise and improve imaging accuracy. In this new method, the pseudo-decoupled wave equations of transverse isotropic (TI) media with a vertical symmetry axis vertical transversely isotropic (VTI) are derived based on the decomposition of the anisotropic elastic stiffness parameters into anisotropic P- and S-wave stiffness parameters. Forward and backward anisotropic P- and S-waves can then be efficiently obtained by numerical solution of the pseudo-decoupled wave equations using the finite difference (FD) method. Combining the vector imaging condition, the high-quality AWSERTM’s results can be obtained. Synthetic examples from the modified HESS VTI model demonstrate the correctness and progressiveness of the proposed method.
高精度迁移技术可降低地震勘探风险。在裂缝发育和沉积地区对各向异性多分量地震数据进行成像具有挑战性。我们在这封信中介绍了一种高效的各向异性波分离弹性反向时间迁移(RTM)技术,用于对各向异性多分量地震数据成像。弹性波被分解成 P 波和 S 波,用于随后的各向异性波分离弹性反演(AWSERTM),以减少串扰噪声,提高成像精度。在这种新方法中,根据将各向异性弹性刚度参数分解为各向异性 P 波和 S 波刚度参数,推导出了具有垂直对称轴垂直横向各向同性(VTI)的横向各向同性(TI)介质的伪解耦波方程。然后,通过使用有限差分(FD)方法对伪解耦(pseudo-decoupled)波方程进行数值求解,可以有效地获得正向和反向各向异性 P 波和 S 波。结合矢量成像条件,可以获得高质量的 AWSERTM 结果。修改后的 HESS VTI 模型的合成示例证明了所提方法的正确性和渐进性。