Annual Report 2000 - WIT
Annual Report 2000 - WIT Annual Report 2000 - WIT
16 CDP number 3100 3000 2900 2800 2700 2600 30 CDP number 3100 3000 2900 2800 2700 2600 25 2.6 20 2.6 15 2.8 10 2.8 5 Time [s] 3.0 0 -5 Time [s] 3.0 3.2 -10 3.2 -15 3.4 -20 3.4 -25 3.6 Detail of optimized CRS stack section (ungained) a) -30 3.6 Difference of emergence angles [°] b) 50 CDP number 3100 3000 2900 2800 2700 2600 50 CDP number 3100 3000 2900 2800 2700 2600 40 2.6 40 2.6 30 30 20 2.8 20 2.8 10 10 0 Time [s] 3.0 0 Time [s] 3.0 -10 3.2 -10 3.2 -20 -20 -30 3.4 -30 3.4 -40 -40 -50 3.6 Detail of 1st emergence angle section [°] c) -50 3.6 Detail of 2nd emergence angle section [°] d) Figure 6: Details of the CRS stack results: a) optimized CRS stack section, c) and d) emergence angles of the first and second detected contributing events, b) difference of the emergence angles shown in c) and d). The steep event in the center of the figures intersects several conflicting events, e.g., the plate boundary in the lower left. Depending on the chosen thresholds for the identification of conflicting dip situations, the intersecting events were detected and characterized. This can be seen best in Figure 6b with the difference of the emergence angles in subfigures c and d. Although the multitude of (actually only sparsely covered) attribute sections is difficult to visualize, we can easily make full use of them to simulate the final ZO section including the interference of intersecting events. Furthermore, the approximate time migration included in the current implementation handles all contributing events separately. In contrast, the conventional post-stack time migration is not able to resolve such ambiguities as its input only contains the superposition of all contributing events.
17 We would like to stress that our proposed approach to handle conflicting dip situations significantly differs from the DMO method: instead of summing along an operator to collect all contributions for all potential dips, we detect and characterize a discrete number of contributing events. Consequently, our approach provides additional wavefield attributes for subsequent applications, whereas DMO corrects the stack result but does not provide any additional information. CONCLUSIONS The pragmatic approach of (Müller, 1998) to perform a ZO simulation by means of the CRS stack method can be adapted to also account for the conflicting dip problem. An additional one-parametric search is required to resolve ambiguities introduced by different events contributing to one and the same ZO sample to be simulated. The consideration of conflicting dips is necessary to obtain a more physical simulation of a ZO section: the simulated interference of intersecting events is closer to the result of an actual ZO measurement. In addition to the improved simulated ZO section, the extended CRS stack strategy provides three kinematic wavefield attributes for each particular event, even if it intersects one or more other events (or its own bow-tie segments). Subsequent applications of these wavefield attributes (e. g., an inversion of the macro-velocity model, calculation of Fresnel zones etc.) benefit from this fact, because otherwise the wavefield attributes in the gaps between “broken” event segments would have to be interpolated. Together with an improved strategy to consider stacking velocity constraints, the extended CRS stack strategy is also better suited to detect and characterize primary events formerly obscured by multiples. The first results obtained with the extended CRS stack strategy demonstrate that the newly introduced features provide a more realistic simulated ZO section as well as a more complete set of wavefield attributes for subsequent applications. We feel that a more adequate selection of the processing parameters, especially concerning the thresholds used to identify conflicting dip situations, will further improve the results. As final remark we would like to indicate that the new CRS stack release which includes all newly introduced features is available for download on the WIT homepage. We would strongly appreciate any feedback concerning the installation and application of this code.
- Page 1 and 2: Wave Inversion Technology WIT Annua
- Page 3: Wave Inversion Technology WIT Wave
- Page 7: Copyright c 2000 by Karlsruhe Unive
- Page 11 and 12: i TABLE OF CONTENTS Reviews: WIT Re
- Page 13 and 14: Wave Inversion Technology, Report N
- Page 15 and 16: 3 theory. It relates properties of
- Page 17: Imaging 5
- Page 20 and 21: 8 two hypothetical eigenwave experi
- Page 22 and 23: 7 ¢¥£§¦©¨ ; < calculate sear
- Page 24 and 25: 7 7 searches ¡ HNJOL for ¢IHNJML
- Page 26 and 27: 14 Trace no. 1000 1500 2000 0.5 1.0
- Page 30 and 31: 18 REFERENCES Höcht, G., de Bazela
- Page 32 and 33: 20 INVERSION BY MEANS OF CRS ATTRIB
- Page 34 and 35: 22 For synthetic data, it is easy t
- Page 36 and 37: — J J J J J J G J - J J G
- Page 39 and 40: Wave Inversion Technology, Report N
- Page 41 and 42: · · v 0 B 0 £ & Ä Ã & v
- Page 43 and 44: 31 Dürbaum, H., 1954, Zur Bestimmu
- Page 45 and 46: Ã Ø Ì 0 0 Ì 4 0 Ã 0 G ' 4
- Page 47 and 48: Wave Inversion Technology, Report N
- Page 49 and 50: 0 0 ˜ ” Z ˜ ” Z 4 4
- Page 51 and 52: 39 strategy by combining global and
- Page 53 and 54: 41 elled data is presented in Figur
- Page 55 and 56: 43 0.2 Distance [m] 1000 1500 2000
- Page 57 and 58: 45 In Figure 10 we have the optimiz
- Page 59: 47 Gelchinsky, B., 1989, Homeomorph
- Page 62 and 63: § ¢ ø ø for a paraxial ray, ref
- Page 64 and 65: Œ § … Z ‹ Z § õ ø \ ø §
- Page 66 and 67: 54 As stated in Hubral and Krey, 19
- Page 68 and 69: § ó § 56 sequence. We made tes
- Page 70 and 71: 58 precision of the modeled input d
- Page 72 and 73: 60 Cohen, J., Hagin, F., and Bleist
- Page 75 and 76: Wave Inversion Technology, Report N
- Page 77 and 78: £ 65 The details of the theory inv
17<br />
We would like to stress that our proposed approach to handle conflicting dip situations<br />
significantly differs from the DMO method: instead of summing along an<br />
operator to collect all contributions for all potential dips, we detect and characterize<br />
a discrete number of contributing events. Consequently, our approach provides additional<br />
wavefield attributes for subsequent applications, whereas DMO corrects the<br />
stack result but does not provide any additional information.<br />
CONCLUSIONS<br />
The pragmatic approach of (Müller, 1998) to perform a ZO simulation by means of<br />
the CRS stack method can be adapted to also account for the conflicting dip problem.<br />
An additional one-parametric search is required to resolve ambiguities introduced by<br />
different events contributing to one and the same ZO sample to be simulated.<br />
The consideration of conflicting dips is necessary to obtain a more physical simulation<br />
of a ZO section: the simulated interference of intersecting events is closer to the<br />
result of an actual ZO measurement.<br />
In addition to the improved simulated ZO section, the extended CRS stack strategy<br />
provides three kinematic wavefield attributes for each particular event, even if it intersects<br />
one or more other events (or its own bow-tie segments). Subsequent applications<br />
of these wavefield attributes (e. g., an inversion of the macro-velocity model, calculation<br />
of Fresnel zones etc.) benefit from this fact, because otherwise the wavefield<br />
attributes in the gaps between “broken” event segments would have to be interpolated.<br />
Together with an improved strategy to consider stacking velocity constraints, the<br />
extended CRS stack strategy is also better suited to detect and characterize primary<br />
events formerly obscured by multiples.<br />
The first results obtained with the extended CRS stack strategy demonstrate that<br />
the newly introduced features provide a more realistic simulated ZO section as well<br />
as a more complete set of wavefield attributes for subsequent applications. We feel<br />
that a more adequate selection of the processing parameters, especially concerning the<br />
thresholds used to identify conflicting dip situations, will further improve the results.<br />
As final remark we would like to indicate that the new CRS stack release which<br />
includes all newly introduced features is available for download on the <strong>WIT</strong> homepage.<br />
We would strongly appreciate any feedback concerning the installation and application<br />
of this code.