Reflection point displacements in transversely isotropic solids

1991 ◽  
Author(s):  
Franklyn K. Levin
Geophysics ◽  
1994 ◽  
Vol 59 (2) ◽  
pp. 309-314 ◽  
Author(s):  
Franklyn K. Levin

One way of representing a subsurface that displays azimuthal anisotropy is to assume transverse isotropy with a horizontal symmetry axis. For solids that can be described in this manner, rays for reflection from a horizontal plane lie in a plane of incidence for P-P, SV-SV, and SH-SH reflection but the plane wave direction generally differs from the ray direction. For P-SV reflections, the reflection points are in the plane of incidence only for profiles parallel to or perpendicular to the symmetry direction. Except for profiles perpendicular to the symmetry direction, P-P and SV-SV moveout velocities have no obvious relation to the travel velocities of the rays.


2006 ◽  
Vol 312 ◽  
pp. 41-46 ◽  
Author(s):  
Bao Lin Wang ◽  
Yiu Wing Mai

This paper solves the penny-shaped crack configuration in transversely isotropic solids with coupled magneto-electro-elastic properties. The crack plane is coincident with the plane of symmetry such that the resulting elastic, electric and magnetic fields are axially symmetric. The mechanical, electrical and magnetical loads are considered separately. Closed-form expressions for the stresses, electric displacements, and magnetic inductions near the crack frontier are given.


1992 ◽  
Vol 27 (1) ◽  
pp. 43-44 ◽  
Author(s):  
P S Theocaris ◽  
T P Philippidis

The basic principle of positive strain energy density of an anisotropic linear or non-linear elastic solid imposes bounds on the values of the stiffness and compliance tensor components. Although rational mathematical structuring of valid intervals for these components is possible and relatively simple, there are mathematical procedures less strictly followed by previous authors, which led to an overestimation of the bounds and misinterpretation of experimental results.


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