Annual Report 2000 - WIT
Annual Report 2000 - WIT Annual Report 2000 - WIT
4 is based on the formulation of these equations as hyperbolic conservation laws and their numerical solution using ENO upwind schemes. Highly accurate traveltimes and smooth amplitudes are obtained which is demonstrated for the Marmousi model. Other Topics The KBC and WHL methods are here compared and applied by Leite et al. to the multiple suppression of peg-legs related to upper low velocity layers (weathering zone), and to deeper high velocity layers (diabase sills).
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- 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
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- Page 15: 3 theory. It relates properties of
- Page 20 and 21: 8 two hypothetical eigenwave experi
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- 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 28 and 29: 16 CDP number 3100 3000 2900 2800 2
- 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
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- Page 43 and 44: 31 Dürbaum, H., 1954, Zur Bestimmu
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- Page 47 and 48: Wave Inversion Technology, Report N
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- 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
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4<br />
is based on the formulation of these equations as hyperbolic conservation laws and<br />
their numerical solution using ENO upwind schemes. Highly accurate traveltimes and<br />
smooth amplitudes are obtained which is demonstrated for the Marmousi model.<br />
Other Topics<br />
The KBC and WHL methods are here compared and applied by Leite et al. to the multiple<br />
suppression of peg-legs related to upper low velocity layers (weathering zone),<br />
and to deeper high velocity layers (diabase sills).
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