Method for estimating shear wave reflection data from acquired compressional wave reflection data

Claim 1

A method of producing shear wave reflection information from compressional wave reflection information comprising the steps of: (a) generating descending acoustic waves from a plurality of acoustic wave sources and receiving and recording at a plurality of receivers ascending waves produced at a subsurface interface; (b) gathering said recorded reflection waves into sets of different source-receiver offsets having a common reflection boundary; (c) correcting said gathered reflection waves for normal moveout; (d) measuring amplitudes of said gathered waves at selected points in time for different source-receiver offset values; (e) determining for each said point in time a component g det which represents the amplitude variations in the measured amplitudes of said gathered waves due to the effects of source-receiver offset; (f) estimating for each said point in time a component of amplitude variation with offset δG which is not due to a shear wave component and is not accounted for in G det ; and (g) determining for each said point in time a shear wave reflectivity component R 3 in accordance with the following: ##EQU11## with P=R.sub.po and Q=GR.sub.po -8T.sup.2 R.sub.so +(2T.sup.2 -1/2)Δρ/ρ, where, R po =normal incident compressional wave reflection coefficient R so =normal incident shear wave reflection coefficient T=average V s /V p , ρ=density G=totality of amplitude effects caused by said variations in the amplitude of the acoustic waves with offset, so that the influence of said amplitude effects on said measured acoustic waves are removed in determining shear wave reflection information.

Claim 2

A method of producing shear wave reflection information from compressional wave reflection information comprising the steps of: (a) generating descending acoustic waves from a plurality of acoustic wave sources and receiving and recording at a plurality of receivers ascending waves produced at a subsurface interface; (b) gathering said recorded reflection waves into sets of different source-receiver offsets having a common reflection boundary; (c) correcting said gathered reflection waves for normal moveout; (d) measuring amplitudes of said gathered waves at selected points in time for different source-receiver offset values; (e) determining for each said point in time a component g det which represents the amplitude variations in the measured amplitudes of said gathered waves due to the effects of source-receiver offset; (f) estimating for each said point in time a component of amplitude variation with offset δG which is not due to a shear wave component and is not accounted for in G det ; and (g) determining for each said point in time a shear wave reflectivity component R 3 in accordance with the following: ##EQU11## with P=R.sub.po and Q=GR.sub.po -8T.sup.2 R.sub.so +(2T.sup.2 -1/2)Δρ/ρ, where, R po =normal incident compressional wave reflection coefficient R so =normal incident shear wave reflection coefficient T=average V s /V p , ρ=density G=totality of amplitude effects caused by said variations in the amplitude of the acoustic waves with offset, so that the influence of said amplitude effects on said measured acoustic waves are removed in determining shear wave reflection information.