PS-wave and P-wave Azimuthal Anisotropy in a Carbonate Basin

B. Mattocks; D. Todorovic-Marinic; J. Li; S.L. Roche; S. Ronen

doi:10.3997/2214-4609-pdb.17.A30

PS-wave and P-wave Azimuthal Anisotropy in a Carbonate Basin
By B. Mattocks, D. Todorovic-Marinic, J. Li, S.L. Roche and S. Ronen
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, EAGE/SEG Research Workshop - Multicomponent Seismic - Past, Present and Future, Sep 2005, cp-17-00030
DOI: https://doi.org/10.3997/2214-4609-pdb.17.A30

Abstract

1 A30 PS-WAVE AND P-WAVE AZIMUTHAL ANISOTROPY IN A CARBONATE BASIN B. MATTOCKS 1 D. TODOROVIC-MARINIC 2 J.LI 1 S. L. ROCHE 1 and S. RONEN 1 1 Veritas DGC Inc. 10300 Town Park Dr Houston TX 77072 USA 2 Veritas GeoServices Summary In an onshore example from a carbonate basin the cumulative PS-wave anisotropy is in good general agreement with regional horizontal stress from borehole breakouts and with symmetry plane orientations determined from azimuthal variations in the AVO gradient of the conventional P-wave 3-D survey. The embedded multicomponent test exhibits all the expected characteristics of converted waves in azimuthally

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2005-09-05

2024-04-19

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PS-wave and P-wave Azimuthal Anisotropy in a Carbonate Basin

Abstract

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The natural combination of full and image‐based waveform inversion

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Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

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Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture