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start [2014/09/10 07:58]
espen
start [2020/10/08 10:49] (current)
knutb [What we do]
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 == News == == News ==
 +  * Abstract to be presented at the EAGE conference in Madrid ({{:raknes_and_weibull_eage2015.pdf|PDF}},{{:chlwang_2015eage.pdf|PDF}}, June 2015)
   * Abstracts of presentation at the SEG conference in Denver ({{:raknes-seg2014-1.pdf|PDF}},{{:raknes-seg2014-2.pdf|PDF}},{{:seg_14_izzie_ref.pdf|PDF}}, October 2014)   * Abstracts of presentation at the SEG conference in Denver ({{:raknes-seg2014-1.pdf|PDF}},{{:raknes-seg2014-2.pdf|PDF}},{{:seg_14_izzie_ref.pdf|PDF}}, October 2014)
   * Article about elastic imaging published and available ({{:raknes-tle-2014.pdf|PDF}},[[http://library.seg.org/doi/abs/10.1190/tle33091000.1|link]], September 2014)   * Article about elastic imaging published and available ({{:raknes-tle-2014.pdf|PDF}},[[http://library.seg.org/doi/abs/10.1190/tle33091000.1|link]], September 2014)
-  * Abstract presented at the EAGE conference in Amsterdam on near-well imaging ({{:Liu2014a.pdf|PDF}}, June 2014)   
-  * An article about time-lapse full-waveform inversion is published and available ({{:raknes2014.pdf|PDF}}, [[http://library.seg.org/doi/abs/10.1190/geo2013-0369.1|link]], May 2014). 
      
  
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 The example below shows images of a channel system at 600m depth obtained with inversion using seismic data recorded at the sea floor. The top row show the true P-wave (left) and S-wave (right) velocity models, whereas the bottom row shows the inverted P- and S-wave velocity models. The example below shows images of a channel system at 600m depth obtained with inversion using seismic data recorded at the sea floor. The top row show the true P-wave (left) and S-wave (right) velocity models, whereas the bottom row shows the inverted P- and S-wave velocity models.
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 {{vp-base-true.png?nolink&250|}}{{vs-base-true.png?nolink&250|}} {{vp-base-true.png?nolink&250|}}{{vs-base-true.png?nolink&250|}}
  
 {{vp-base-inv.png?nolink&250}}{{vs-base-inv.png?nolink&250}} {{vp-base-inv.png?nolink&250}}{{vs-base-inv.png?nolink&250}}
  
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 Time-lapse seismic inversion is a rather new application of the method. The purpose of the application is to reveal changes in time in the subsurface due to for instance production or injection of CO2. The left figure below show the true time-lapse effect in the channel system, whereas the right figure show the time-lapse effect obtained using inversion. Time-lapse seismic inversion is a rather new application of the method. The purpose of the application is to reveal changes in time in the subsurface due to for instance production or injection of CO2. The left figure below show the true time-lapse effect in the channel system, whereas the right figure show the time-lapse effect obtained using inversion.
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 {{true-tl.png?nolink&400}}{{tl-vp.png?nolink&400}} {{true-tl.png?nolink&400}}{{tl-vp.png?nolink&400}}
  
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 === Information === === Information ===
-The projects we work on are part of the [[http://www.ipt.ntnu.no/rosewiki/ | ROSE ]] consortium.+The projects we work on are part of the [[http://www.ipt.ntnu.no/rose/ | ROSE ]] consortium.
  
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-~~DISCUSSION:off~~ 
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start.1410335897.txt.gz · Last modified: 2014/09/10 07:58 by espen
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