S. Stokes, D. Manns, M. Romanenko, B. Kjølhamar, R. Myklebust, E. Henden
{"title":"挪威巴伦支海Senja Ridge的FWI速度模型构建工作流程","authors":"S. Stokes, D. Manns, M. Romanenko, B. Kjølhamar, R. Myklebust, E. Henden","doi":"10.3997/2214-4609.201900030","DOIUrl":null,"url":null,"abstract":"Summary The Senja Ridge is a structurally complex high located in the western margin of the Norwegian Barents Sea. A two stage velocity model building approach is implemented, utilising diving wave FWI and high resolution image guided tomography. Shallow gas clouds and shallow channels are resolved with the FWI updates, deeper structures including basement horsts within the Senja Ridge and the flanks of salt diapirs are solved with the tomographic updates.","PeriodicalId":350524,"journal":{"name":"Second EAGE/PESGB Workshop on Velocities","volume":"23 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-04-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A FWI Velocity Model Building Workflow across the Senja Ridge in the Norwegian Barents Sea\",\"authors\":\"S. Stokes, D. Manns, M. Romanenko, B. Kjølhamar, R. Myklebust, E. Henden\",\"doi\":\"10.3997/2214-4609.201900030\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Summary The Senja Ridge is a structurally complex high located in the western margin of the Norwegian Barents Sea. A two stage velocity model building approach is implemented, utilising diving wave FWI and high resolution image guided tomography. Shallow gas clouds and shallow channels are resolved with the FWI updates, deeper structures including basement horsts within the Senja Ridge and the flanks of salt diapirs are solved with the tomographic updates.\",\"PeriodicalId\":350524,\"journal\":{\"name\":\"Second EAGE/PESGB Workshop on Velocities\",\"volume\":\"23 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2019-04-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Second EAGE/PESGB Workshop on Velocities\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.3997/2214-4609.201900030\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Second EAGE/PESGB Workshop on Velocities","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609.201900030","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
A FWI Velocity Model Building Workflow across the Senja Ridge in the Norwegian Barents Sea
Summary The Senja Ridge is a structurally complex high located in the western margin of the Norwegian Barents Sea. A two stage velocity model building approach is implemented, utilising diving wave FWI and high resolution image guided tomography. Shallow gas clouds and shallow channels are resolved with the FWI updates, deeper structures including basement horsts within the Senja Ridge and the flanks of salt diapirs are solved with the tomographic updates.
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