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Vladimir Grechka Shell International E&P

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Presentation on theme: "Vladimir Grechka Shell International E&P"— Presentation transcript:

1 Vladimir Grechka Shell International E&P
S-wave processing Vladimir Grechka Shell International E&P Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

2 Reflected PS-wave Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

3 Complications of PS-wave data
• moveout asymmetry • polarity reversal • conversion point dispersal no standard processing flow Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

4 PP + PS = SS method (Grechka and Tsvankin, 2001)
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

5 PP + PS = SS method Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

6 PP + PS = SS method Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

7 PP + PS = SS method • PP and PS event correspondence
 accurate velocity and anisotropy model not needed • prestack traveltime picking Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

8 PP + PS = SS method • PP and PS event correspondence
 accurate velocity and anisotropy model not needed • prestack traveltime picking Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

9 PP + PS = SS method • PP and PS event correspondence
 accurate velocity and anisotropy model not needed • prestack traveltime picking • convolution of PP and PS traces Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

10 PP + PS = SS method • PP and PS event correspondence
 accurate velocity and anisotropy model not needed • prestack traveltime picking • convolution of PP and PS traces ΨS data suitable for S-wave velocity analysis Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

11 ΨS-wave data • integration over all P-wave source and PP data in
reverse time • integration over all P-wave source and receiver locations Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

12 Synthetic example Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

13 Input PP and PS data • PS moveout asymmetry
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

14 Input PP and PS data (zoom)
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

15 Input PP and PS data (zoom)
• polarity reversal Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

16 Input PP and PS data (zoom)
• polarity reversal • different PP and PS wavelets Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

17 Generated ΨS data Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

18 Generated ΨS data • correct traveltimes of ΨS arrivals
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

19 Generated ΨS data (zoom 1)
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

20 Generated ΨS data (zoom 1)
• longer ΨS wavelets Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

21 Generated ΨS data (zoom 1)
• longer ΨS wavelets • no polarity reversal Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

22 Generated ΨS data (zoom 1)
• longer ΨS wavelets • no polarity reversal • almost zero ΨS trace at zero offset Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

23 Generated ΨS data (zoom 2)
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

24 Generated ΨS data (zoom 2)
• ΨS-waves cannot be reconstructed at large offsets Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

25 Generated ΨS data (zoom 2)
• ΨS-waves cannot be reconstructed at large offsets  critical angle Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

26 Critical offset for ΨS-waves
P P R critical ray Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

27 Critical offset for ΨS-waves
P P R critical ray Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

28 Critical offset for ΨS-waves
P P R critical ray Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

29 Gulf of Mexico (PP-waves, shallow)
offset = depth Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

30 Gulf of Mexico (ΨS-waves, shallow)
offset = depth Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

31 Gulf of Mexico (PP-waves, deep)
offset = depth Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

32 Gulf of Mexico (ΨS-waves, deep)
offset = depth Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

33 PP- and ΨS-wave gathers
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

34 Evidence for effective anisotropy
• in homogeneous VTI media • isotropy does not fit data Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

35 Conclusions (I) • complications of PS-wave data irrelevant
 moveout asymmetry  polarity reversal  conversion point dispersal Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

36 Conclusions (II) • ΨS data ideal for S-wave velocity analysis
• accuracy of shear-wave stacking velocities governed by the ratio • straightforward estimating of effective anisotropy Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

37 Further opportunities
Issues • absence of P-wave data (gas chimneys) • event correspondence Further opportunities • post-critical S events = diving P-waves • amplitudes • migration of S data Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

38 Acknowledgements • Helmut Jakubowicz (Veritas) • Joe Dellinger (BP)
• Chris Corcoran, Fons ten Kroode, Jon Sheiman, Allen Hillery, Jared Martin, Mark Zama, Paul Milcik, Barbara Yantis, Richard Cook (Shell) • Pawan Dewangan (CSM) Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

39 Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

40 Appendix Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

41 ΨS-wave data • integration over all P-wave source and PP data in
reverse time • integration over all P-wave source and receiver locations Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

42 Spectrum of ΨS trace Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

43 Spectrum of ΨS trace (single event)
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

44 Spectrum of ΨS trace (single event)
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

45 Stationary phase conditions
= matching of PP and PS reflection slopes Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

46 Phase at stationary point
• kinematics of pure-S primary Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

47 Spectrum of ΨS trace in 3-D
Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002

48 Grechka, V., S-wave processing: Force Seminar “4C/OBS Data Processing and Interpretation – Old Myths, New Insights,” Stavanger, Norway, April 22, 2002


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