To: “A physical model of shear wave propagation in transversely isotropic solid,” by Chih‐Hsiung Chang, G. H. F. Gardner, and John A. McDonald (March 1994 GEOPHYSICS, 59, p. 484–487)

Geophysics ◽  
1994 ◽  
Vol 59 (8) ◽  
pp. 1311-1311
Keyword(s):  
Wave Propagation ◽  
Physical Model ◽  
Shear Wave ◽  
Transversely Isotropic ◽  
Isotropic Solid ◽  
Model Study

The title of this paper was incorrect. The title should be, “A physical model study of shear wave propagation in transversely isotropic solid.”

A physical model of shear‐wave propagation in a transversely isotropic solid

Geophysics ◽  
1994 ◽  
Vol 59 (3) ◽  
pp. 484-487 ◽  
Author(s):  
Chih‐Hsiung Chang ◽  
G. H. F. Gardner ◽  
John A. McDonald
Keyword(s):  
Wave Propagation ◽  
Physical Model ◽  
Shear Wave ◽  
Seismic Anisotropy ◽  
Sedimentary Rocks ◽  
Physical Property ◽  
Transversely Isotropic ◽  
Velocity Variation ◽  
Common Phenomenon ◽  
Isotropic Solid

It is now understood that seismic anisotropy is a comparatively common phenomenon in sedimentary layers. The elastic properties of most sedimentary rocks have been shown to be anisotropic. (Anisotropy means that the physical property of the material is a function of the measuring direction). Seismologists are generally concerned with velocity variation with the direction of propagation.

A physical model study of shear wave splitting and fracture intensity

1987 ◽  
Author(s):  
Robert H. Tatham ◽  
Martin D. Matthews ◽  
K. K. Sekharan ◽  
Christopher J. Wade ◽  
Louis M. Liro
Keyword(s):  
Physical Model ◽  
Shear Wave ◽  
Shear Wave Splitting ◽  
Model Study ◽  
Wave Splitting ◽  
Fracture Intensity

A Physical Model Study of Shear-Wave Splitting and Fracture Intensity

1988 ◽  
Vol 19 (1-2) ◽  
pp. 175-178 ◽  
Author(s):  
Robert H. Tatham ◽  
Martin D. Matthews ◽  
K. K. Sekharan
Keyword(s):  
Physical Model ◽  
Shear Wave ◽  
Shear Wave Splitting ◽  
Model Study ◽  
Wave Splitting ◽  
Fracture Intensity
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