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The APPEA Journal The APPEA Journal Society
Journal of Australian Energy Producers
RESEARCH ARTICLE (Non peer reviewed)

Automatic NMO correction in anisotropic media and non-hyperbolic NMO velocity field estimation

Mohamed Sedek A and Lutz Gross A
+ Author Affiliations
- Author Affiliations

School of Earth Sciences, The University of Queensland.

The APPEA Journal 56(2) 592-592 https://doi.org/10.1071/AJ15098
Published: 2016

Abstract

The authors propose a new method to automatically normal move-out correct pre-stack seismic reflection data that is sorted by CDP gathers, and to estimate the normal move-out (NMO) velocity (Vnmo) as a full common depth point (CDP) velocity field that instantaneously varies with offsets/azimuths.

The method is based on doing a pre-defined number of NMO velocity iterations using linear vertical interpolation of different NMO velocities at each seismic trace individually. At each iteration the seismic trace is shifted and multiplied by the zero offset trace followed by the summation of the product. Then, after all the iterations are done, the one with the maximum summation value is chosen, which is assumed to be the most suitable NMO velocity trace that accurately flattens seismic reflection events. The other traces follow the same process, and a final velocity field is then extracted.

Another new, simple and fast method is also introduced to estimate the anisotropic effect from the extracted NMO velocity field. The method runs by calculating the spatial variation of the estimated NMO velocities at each arrival time and offset/azimuth, therefore instantaneously estimating the anisotropic effect.

Isotropic and anisotropic synthetic geological models were built based on a ray-tracing algorithm to test the method. A range of synthetic background noise was applied, starting from 10–30%. The method has also been tested on Hess’s model and coal seam gas field data CDP examples. An Alaskan pre-stack seismic CDP field example has also been used.

Mohamed Sedek is a PhD scholar at the School of Earth Sciences’ Centre for Geoscience Computing, at The University of Queensland. From 2006–07 he was a Geophysicist at Spectrum Seismic, a data processing company. Mohamed was a teaching assistant at the Geophysics department at Cairo University from 2007–12, and an assistant lecturer there from 2012–15, where he worked on different projects for local and international oil companies. He received his Bachelor’s degree from the Geophysics department at Cairo University in 2006.

Lutz Gross has been an Associate Professor at The University of Queensland’s School of Earth Sciences since 2003. Before his appointment at UQ, Lutz was a Computational Scientist in the CSIRO’s Mathematical and Information Sciences Division in Melbourne from 2001–03, and a lecturer at the Institute of Information and Mathematical Sciences at Massey University (Albany, New Zealand) from 2000–01. He has also worked at the Centre for Mathematics and its Applications at the Australian National University’s School of Mathematical Sciences (Canberra) as a Research Fellow from 1996–99, and was a Research Scientist at the University of Karlsruhe’s Computing Centre (Germany) from 1989–96.


References

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Baan, M., and Kendall, J. (2002). Estimating anisotropy parameters and traveltimes in the -p domain. Geophysics 67, 1076–86.

Stockwell, J.J.W, 2011—Seismic Un*x release No.8. Center for Wave Phenomena, Colorado School of Mines, 8, 269–71.

Thomsen, L. (1986). Weak elastic anisotropy. Geophysics 51, 1954–66.

Tsvankin, I., 1998—Influence of seismic anisotropy on velocity analysis and depth imaging: in Model-Based Depth Imaging by S. Fagin, SEG.

Tsvankin, I., and Thomsen, L. (1995). Inversion of reflection traveltimes for transverse isotropy. Geophysics 60, 1095–107.