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Application of Finite-Difference Method in Modelling an Oil Bearing Structure


Affiliations
1 National Geophysical Research Institute, Hyderabad - 500 007, India
     

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Finite-difference numerical technique has been in use for over two decades in solving elastic wave equation for the interpretation of seismic response of complex 2-D and to a limited extent, 3-D oil bearing geological structures. The present communication consists of two parts. In the first part, synthetic seismograms have been obtained under plane wave as well as line source excitations for a gas cap structure and over a salt dome/basement undulation. In the second part, seismogram under plane wave conditions has been computed for a geological structure from the Gujarat coast. Some of the faults confining the pay zone between 1800 ms and 1900 ms in the time section are highlighted.

Keywords

Seismology, Structure, Hydrocarbon, Gujarat.
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  • Application of Finite-Difference Method in Modelling an Oil Bearing Structure

Abstract Views: 181  |  PDF Views: 1

Authors

B. S. Rathor
National Geophysical Research Institute, Hyderabad - 500 007, India
M. Devanandam
National Geophysical Research Institute, Hyderabad - 500 007, India
K. Mallick
National Geophysical Research Institute, Hyderabad - 500 007, India

Abstract


Finite-difference numerical technique has been in use for over two decades in solving elastic wave equation for the interpretation of seismic response of complex 2-D and to a limited extent, 3-D oil bearing geological structures. The present communication consists of two parts. In the first part, synthetic seismograms have been obtained under plane wave as well as line source excitations for a gas cap structure and over a salt dome/basement undulation. In the second part, seismogram under plane wave conditions has been computed for a geological structure from the Gujarat coast. Some of the faults confining the pay zone between 1800 ms and 1900 ms in the time section are highlighted.

Keywords


Seismology, Structure, Hydrocarbon, Gujarat.