Seismic Intro
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![Page 1: Seismic Intro](https://reader034.fdocuments.us/reader034/viewer/2022042608/55cf92b1550346f57b98cbc0/html5/thumbnails/1.jpg)
Just Enough Seismic . . .
to get in trouble
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A Bit of Physics• Acoustic Impedance = Velocity X Density• Reflections occur where there is an impedance
contrast between two rock layers• ~0.01% of the seismic wave is reflected• Interval seismic velocities generally increase with
depth– 10 msec at 1 sec TWT represents less rock than 10
msec at 2 sec TWT
Unmigrated seismic data is displayed relative to thereceivers
Migrated seismic data is displayed relative to the Earth
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http://www.glossary.oilfield.slb.com/DisplayImage.cfm?ID=210
Acoustic Impedence = Velocity X Density
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•Interval seismic velocities generally increase with depth•10 msec at 1 km represents less rock than 10 msec at 2 km
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Seismic data is subject to much computer processing
After today we will use Migrated Data in our exercises.
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UNMIGRATED
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