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dc.contributor.authorLi, Xu
dc.contributor.authorSze, Edmond
dc.contributor.authorBurns, Daniel R.
dc.contributor.authorToksoz, M. Nafi
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-01-20T18:11:04Z
dc.date.available2012-01-20T18:11:04Z
dc.date.issued2004
dc.identifier.urihttp://hdl.handle.net/1721.1/68617
dc.description.abstractFrom polarization analysis on a covariance matrix, a method of S-wave splitting analysis is developed, which processes 3-component recordings simultaneously, rather than just 2 horizontal components as done traditionally. Thus not only orientation, but also dip information of fractures can be resolved. The synthetic test results show that this method is stable even for noise levels as high as 100% (S/N=1). If time window sizes are larger than roughly twice the time delay between the fast and slow S waves, the results are always reasonable even with noise levels up to 50%.The method is applied to 12 microseismic events recorded from a producing reservoir. The preliminary results suggest that stress-aligned fractures strike in NE-SW direction in the reservoir. The dips of the fractures are primarily vertical. The time difference between the fast and slow shear waves is about several tens of milliseconds per kilometer.en_US
dc.description.sponsorshipUnited States. Dept. of Energy (grant DE.FC03-015F22398)en_US
dc.description.sponsorshipMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.publisherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.relation.ispartofseriesEarth Resources Laboratory Industry Consortia Annual Report;2004-06
dc.titleS-wave Splitting Analysis: Covariance Matrix Method and Preliminary Applicationen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorLi, Xu
dc.contributor.mitauthorSze, Edmond
dc.contributor.mitauthorBurns, Daniel R.
dc.contributor.mitauthorToksoz, M. Nafi
dspace.orderedauthorsLi, Xu; Sze, Edmond; Burns, Daniel R.; Toksoz, M. Nafien_US


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