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Salt Boundary Delineation by Transmitted PS Waves David Sheley
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Outline MotivationMotivation Transmission Migration TheoryTransmission Migration Theory ResultsResults –Synthetic –Gulf of Mexico VSP ConclusionsConclusions
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Problem: Limited Illumination SEDIMENT Receiver Well SEDIMENT P PP SALT
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Solution: PS Transmission Migration SEDIMENT PS Receiver Well SEDIMENT P SALT
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Outline MotivationMotivation Transmission Migration TheoryTransmission Migration Theory ResultsResults –Synthetic –Gulf of Mexico VSP ConclusionsConclusions
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Conventional PP Migration m(r) = S(z g, sr + rg ) sr rg s r g
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m(r) = S(z g, sr + rg ) sr s r g Transmission PS Migration rg P-wave S-wave
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m(r) = S(z g, sr + rg ) sr s r g Transmission PS Migration rg
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Outline MotivationMotivation Transmission Migration TheoryTransmission Migration Theory ResultsResults –Synthetic –Gulf of Mexico VSP ConclusionsConclusions
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Depth (m) Offset (m) 1000 100 0 ds = 1 m dg = 1 m Vertical Boundary RVSP Model V = 5500 m/s P V = 5000 m/s P V = 3333 m/s S V = 3666 m/s S Source = 1500 Hz
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Synthetic RVSP Data 0 One-way Traveltime (ms) 20 40 60 Offset (m) 1000
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Synthetic RVSP Data 0 One-way Traveltime (ms) 20 40 60 Offset (m) 1000 Direct P PS Direct S SP PS PP SP
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Depth (m) Offset (m) 1000 100 0 PP Reflection Migration P PP
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PP Reflection Kirchhoff Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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PP Kirchhoff Migration: 90% Velocity Depth (m) Offset (m) 0 100 0 100 Reduced-TimeConventional Depth (m) Offset (m) 0 100 0 100
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PP Reflection Wavepath Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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PP Wavepath Migration: 90% Velocity Depth (m) Offset (m) 0 100 0 100 Reduced-TimeConventional Depth (m) Offset (m) 0 100 0 100
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Depth (m) Offset (m) 1000 100 0 PS Transmission Migration PS P
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PS Transmission Kirchhoff Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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PS Kirchhoff Migration: 90% Velocity Depth (m) Offset (m) 0 100 0 100 Reduced-TimeConventional Depth (m) Offset (m) 0 100 0 100
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PS Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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PS Wavepath Migration: 90% Velocity Depth (m) Offset (m) 0 100 0 100 Reduced-TimeConventional Depth (m) Offset (m) 0 100 0 100
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Depth (m) Offset (m) 1000 100 0 SP Transmission Migration S SP
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SP Transmission Kirchhoff Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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SP Kirchhoff Migration: 90% Velocity Depth (m) Offset (m) 0 100 0 100 Reduced-TimeConventional Depth (m) Offset (m) 0 100 0 100
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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SP Wavepath Migration: 90% Velocity Depth (m) Offset (m) 0 100 0 100 Reduced-TimeConventional Depth (m) Offset (m) 0 100 0 100
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SP Transmission Kirchhoff Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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SP Transmission Kirchhoff Migration Depth (m) Offset (m) 0 100 0 100 True Velocity Single Gather Depth (m) Offset (m) 0 100 0 100
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SP Transmission Kirchhoff Migration Depth (m) Offset (m) 0 100 0 100 90% Velocity Depth (m) Offset (m) 0 100 0 100 Single Gather
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True Velocity Depth (m) Offset (m) 0 100 0 100 SP Transmission Kirchhoff Migration 90% Velocity Depth (m) Offset (m) 0 100 0 100
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 Depth (m) Offset (m) 0 100 0 100 KM Single Gather True Velocity
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 Depth (m) Offset (m) 0 100 0 100 Ray Tracing True Velocity
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 Depth (m) Offset (m) 0 100 0 100 Fresnel Zone True Velocity
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 Depth (m) Offset (m) 0 100 0 100 Wavepath Image True Velocity
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 True Velocity 90% Velocity Depth (m) Offset (m) 0 100 0 100
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 90% Velocity Depth (m) Offset (m) 0 100 0 100 KM Single Gather
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 Depth (m) Offset (m) 0 100 0 100 Ray Tracing 90% Velocity
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 Depth (m) Offset (m) 0 100 0 100 Fresnel Zone 90% Velocity
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SP Transmission Wavepath Migration Depth (m) Offset (m) 0 100 0 100 Depth (m) Offset (m) 0 100 0 100 Wavepath Image 90% Velocity
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Outline MotivationMotivation Transmission Migration TheoryTransmission Migration Theory ResultsResults –Synthetic –Gulf of Mexico VSP ConclusionsConclusions
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Acquisition Geometry Depth (kft) Offset (kft) 4 0 8 12 4 SALT Depth (kft) Offset (kft) 4 0 8 12 4 SALT
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P-Wave Velocity Depth (kft) Offset (kft) 150 4 0 8 12 4 5 0 Velocity (kft/s) 5 15 Depth (kft) 0 4 8 12 10
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S-Wave Velocity Depth (kft) Offset (kft) 150 4 0 8 12 4 5 0 Velocity (kft/s) 5 15 Depth (kft) 0 4 8 12 10
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Offset 500 ft Z-Component Depth (ft) 8700 12900 One-way Traveltime (s) 1.81.42.22.6 SALT Direct P Reflected P
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500 ft Offset: PP Reflections Depth (ft) 8700 12900 One-way Traveltime (s) 1.81.42.22.6 SALT
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500 ft Depth (ft) 8000 14700 2000 ft Synthetic 8000 14700 SALTSALT PP Reflection Migration Receivers Receivers
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Offset 500 ft X-Component Depth (ft) 8700 12900 One-way Traveltime (s) 1.81.42.22.6 SALT Reflected PS Direct P
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500 ft Offset: PS Reflections Depth (ft) 8700 12900 One-way Traveltime (s) 1.81.42.22.6 SALT
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500 ft Depth (ft) 8000 14700 2000 ft Synthetic 8000 PS Reflection Migration Receivers Receivers 14700 SALTSALT
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Offset 500 ft X-Component Depth (ft) 8700 12900 One-way Traveltime (s) 1.81.42.22.6 SALT Direct P Transmitted PS
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500 ft Offset: PS Transmissions Depth (ft) 8700 12900 One-way Traveltime (s) 1.81.42.22.6 SALT
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500 ft Depth (ft) 8000 14700 2000 ft Synthetic 8000 PS Transmission Migration Receivers Receivers 14700 SALTSALT
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Outline MotivationMotivation Transmission Migration TheoryTransmission Migration Theory ResultsResults –Synthetic –Gulf of Mexico VSP ConclusionsConclusions
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Conclusions Reduced-time is shown to reduce migration errors in PP reflection images.Reduced-time is shown to reduce migration errors in PP reflection images. The top and bottom of the salt tablet were successfully imaged using the three VSP gathers.The top and bottom of the salt tablet were successfully imaged using the three VSP gathers. PS transmission migration sucessfully imaged a tranmitting boundary above the receiver array.PS transmission migration sucessfully imaged a tranmitting boundary above the receiver array.
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Implications Can vertical salt boundaries be imaged using PS transmissions.Can vertical salt boundaries be imaged using PS transmissions. VSP transmission migraion an alternative to single well imaging ?VSP transmission migraion an alternative to single well imaging ? Greater illumination using combined PP reflection and PS transmissionsGreater illumination using combined PP reflection and PS transmissions = Cheaper VSP. = Cheaper VSP.
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