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Just Enough Seismic . . . to get in trouble

Intro to Seismic Interpretation

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Page 1: Intro to Seismic Interpretation

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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