Abstract

P-S converted seismic wave exploration plays an important role in detecting complex geologic structures. In this research, we derive two new asymptotic conversion point equations for the P-S converted wave reflected from a dipping reflector. The first is a quadratic asymptotic conversion point equation of the P-S converted wave reflection from a dipping reflector (DACP equation), and the second is a linear asymptotic equation (ADACP equation). DACP and ADACP equations depend on the velocity ratio (VP/VS) of the stratum, the offset (X), the depth (Z) of the conversion point, and the dip angle of the stratum. The last parameter is the most sensitive of the DACP and ADACP equations in determining the conversion point position. The two new equations can predict the conversion point positions on a deep dipping reflector accurately and directly. The accuracy of the conversion point position at shallow depth determined by the DACP equation is better than using the ADACP equation. For a shallow conversion point, for example Z/X = 0.5, the errors of the conversion point prediction in the horizontal distance (CP error) are less than 2% for the DACP equation, but the CP errors are very large for the ADACP equation. If Z/X is greater than 3, the CP errors of the ADACP equation are less than 3% and this equation is more computationally efficient than the DACP equation.

Highlights

  • P wave reflection seismology has been successfully applied in oil exploration in resent years

  • Chang and Tang (2005) extended the conversion point (CP) equation and derived a new quartic equation (DCP equation) for the P-S converted wave reflected from a dipping reflector

  • From the ACP equation for the P-S converted wave reflected from a dipping reflector

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Summary

Introduction

P wave reflection seismology has been successfully applied in oil exploration in resent years. Chang and Tang (2005) extended the CP equation and derived a new quartic equation (DCP equation) for the P-S converted wave reflected from a dipping reflector. A converted wave’s DMO (dip move-out) equation can calculate the travel time of a P-S converted wave reflected from an isotropic stratum with a dipping reflector (Ikelle and Amundsen 2005) It can not determine the CP position on a dipping reflector. We will derive new asymptotic equations of the DCP equation for the deep reflected P-S converted wave These equations will be more computationally efficient and direct in resolving the CP position for the P-S converted wave reflected from a deep dipping reflector

Asymptotic conversion point equations
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