Seismic anisotropy in sedimentary rocks, part 1: A single‐plug laboratory method

Author:

Wang Zhijing1

Affiliation:

1. ChevronTexaco Exploration & Production Technology Co., P.O. Box 6019, San Ramon, California 94583‐0719.

Abstract

A single‐plug method for measuring seismic velocities and transverse isotropy in rocks has been rigorously validated and laboratory tested. The method requires only one sample to measure the velocities needed to derive the five independent elastic constants for transversely isotropic materials. In this method, piezoelectric transducers are fitted to the top, bottom, and sides of the cylindrical sample. Laboratory velocity and anisotropy can be measured as functions of pressure, temperature, fluid saturation, and fluid displacement. Because this method uses a horizontal core plug that has much higher permeability than a vertical core plug, it is especially suitable for low‐permeability shale measurements. It reduces the sample preparation and velocity measurement time by more than two‐thirds.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference5 articles.

1. Lin, W., 1985, Ultrasonic velocities and dynamic elastic moduli of Mesaverde rocks: Lawrence Livermore National Laboratory Report UCID‐20273.

2. Shear‐wave velocity anisotropy in sedimentary rocks: A laboratory study

3. Vernik, L., Liu, X., and Nur, A., 1994, Effect of kerogen on velocity anisotropy in source rocks: 64th Ann. Internat. Mtg., Soc. Expl. Geophys., Expanded Abstracts, 323–326.

4. Seismic anisotropy in sedimentary rocks, part 2: Laboratory data

5. Yin, H., 1992, Acoustic velocity and attenuation of rocks: Isotropy, intrinsic anisotropy, and stress induced anisotropy: Ph.D. thesis, Stanford Univ.

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