{"title":"Q-Compensation by Least Squares Migration","authors":"G. Xia, R. Crider","doi":"10.3997/2214-4609-pdb.3.p007","DOIUrl":null,"url":null,"abstract":"P007 Q-COMPENSATION BY LEAST SQUARES MIGRATION Summary 1 An efficient and stable poststack Q compensation method based on wavefield extrapolation and migration principle is presented. Our inverse Q filter compensates for both amplitude decay and phase dispersion and handles detailed Q variation with depth. A least squares extrapolation operator is used to stabilize the inverse filter. A real data example of Q compensation application shows higher resolution balanced spectrum and improved well ties. Introduction The earth absorbs energy as sound waves travel through. In seismic experiments wave scattering and inter-bed multiples also contribute to attenuation (O’Doherty & Anstey 1971). Regardless","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"98 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"66th EAGE Conference & Exhibition","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609-pdb.3.p007","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
P007 Q-COMPENSATION BY LEAST SQUARES MIGRATION Summary 1 An efficient and stable poststack Q compensation method based on wavefield extrapolation and migration principle is presented. Our inverse Q filter compensates for both amplitude decay and phase dispersion and handles detailed Q variation with depth. A least squares extrapolation operator is used to stabilize the inverse filter. A real data example of Q compensation application shows higher resolution balanced spectrum and improved well ties. Introduction The earth absorbs energy as sound waves travel through. In seismic experiments wave scattering and inter-bed multiples also contribute to attenuation (O’Doherty & Anstey 1971). Regardless