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Basic Seismic Processing INPUT FILTER CMP Gather NMO STACK MIGRATE DISPLAY GEOM VEL ANAL STATICS MUTE.

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Presentation on theme: "Basic Seismic Processing INPUT FILTER CMP Gather NMO STACK MIGRATE DISPLAY GEOM VEL ANAL STATICS MUTE."— Presentation transcript:

1 Basic Seismic Processing INPUT FILTER CMP Gather NMO STACK MIGRATE DISPLAY GEOM VEL ANAL STATICS MUTE

2 More Seismic Processing INPUT BP FILTER CMP Gather NMO STACK MIGRATE DISPLAY GEOM VEL ANAL STATICS DEMUX VIB CORR FK FILTER DECON DMO/ MIGRATE SAVE DECON FK FILTER MUTE GAIN RCVR COHERENCY ENHANCE COHERENCY ENHANCE TIME TO DEPTH EDIT

3 Stack

4 Migration actual Seismic section (unmigrated) Migration (move it back) sin(  ) = tan (  ), where  = true dip,  = apparent dip

5 Migration: Syncline

6 Migration Effects Models (perfectly migrated) Synthetic Seismic Sections (Unmigrated)

7 Diffraction Point Reflector (Diffractor) Reflection Response (Diffraction)

8 Diffraction Model of Generic Reflection Multiple diffractors  x = finite Multiple diffractors  x 0

9 Migration with Velocity Distortion Layer 1 Layer 2 Layer 3 ALL

10 Depth Migration & Stack Smearing Zero-0ffset (Single fold) 10 Fold Stack

11 Migration Ex: Syncline Before After Migration ?

12 Migration Ex: Fault Before MigrationAfter Migration

13 Migration Example Before Migration After Migration

14 Migration: Methodology Diffraction Summation (Diffraction Stack) Wavefront Summation (Kirchoff Stack) unmigrated migrated

15 Migration Methodology Exploding Reflector (Back Propagation, Wave Equation Finite Difference, FK)

16 Migration Artifacts: Aperture 35 traces 70 traces 150 traces 256 traces

17 Migration Artifacts: Velocity Migration Artifacts: Velocity True V V 5% low V 10% low V 20% low

18 Migration and Noise Random Noise + Migration Migration “smiles” esp at edges of data Unmigrated Migrated

19 Migration: Voila Note: Steep dip migration


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