Abstract

Modification of the hyperbolic travel time equation into non-hyperbolic travel time equation is important to increase the reduction residual moveout for long offset data. Some researchers have modified hyperbolic travel time equation into a non-hyperbolic travel time equation to obtain a more accurate value NMO velocity and parameter an-ellipticity or etha on the large offset to depth ratio (ODR) so that the residual moveout value is smaller mainly in large offset to depth ratio. The aims of research is to increase the reduction value of error residue at long offset data using Padé approximation then compare with several approximations. The method used in this study is to conduct forward modeling of the subsurface coating structure. The results of the three-dimensional analysis show that the Padé approximation has the best accuracy compared to the other travel time equations for ODR value up to 4 with an-ellipticity parameter is varying from 0 to 0.5. Testing of synthetic data for single layer on vertical transverse isotropy (VTI) medium obtained the maximum residual error value produced by the Padé approximation is 0.25% in ODR=4. Therefore, Padé approximation is better than other methods for reducing residual moveout.

Highlights

  • Technology in oil and gas sector in Indonesia is not good enough

  • Anisotropic properties of rocks can be seen at the Normal Moveout (NMO) correction

  • The aim of NMO correction to eliminate the effect of distance

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Summary

Introduction

Technology in oil and gas sector in Indonesia is not good enough. Some of the factors needed to find new oil reserves are to add information from seismic data obtained. Processing and interpretation of seismic data usually assume a homogeneous isotropy medium. The real subsurface are generally heterogeneous anisotropy medium. Anisotropic properties of rocks can be seen at the Normal Moveout (NMO) correction. The aim of NMO correction to eliminate the effect of distance. The NMO correction depends on offset and velocity. The problem caused when Normal Moveout (NMO) correction is the stretching effect. The trigger for stretching effect is influenced by frequency attenuation of seismic waves experienced by incoming ray velocity received at a far offset [1]

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