definition
Seismic anisotropy is the speed of propagation of seismic waves in a medium with particles polarization direction related.
Physical mechanism
Most mineral crystals in nature are anisotropic, and this anisotropy is microscopic anisotropy. When a large number of anisotropic crystals are randomly arranged, they exhibit macroscopically isotropic characteristics.
There are two mechanisms for macroscopic anisotropy:
- LPO (lattice-preferred orientation): The mineral crystal itself is anisotropic, forming macroscopic anisotropy due to the orientation of crystal particles.
- SPO (shape-preferred orientation): Orientation of isotropic media with different wave velocities causes macroscopic anisotropy
The anisotropy and inhomogeneity of the medium are completely different concepts. Anisotropy describes the change of media properties at a certain point with direction. The non-uniformity describes the difference in properties of media between two points.
Anisotropic classification:
- An isotropic medium, the elastic parameter requires two parameter representations
- VTI, Vertical Transverse Isotropy, the axis of anisotropic symmetry is vertical, and the different directions in the horizontal plane are isotropic. The elastic parameters need to be represented by 5 parameters. The common VTI is caused by media layering.
- HTI, Horizontal Transverse Isotropy, the axis of anisotropic symmetry is horizontal, and the different directions in the vertical plane are isotropic. The elastic parameters need to be represented by 5 parameters. The common HTI is caused by vertical cracks.
- TTI, Tilted Transverse Isotropy, tilt anisotropy, anisotropic symmetry axis is oblique
- Fully anisotropic media, elastic parameters require 21 parameters
Anisotropy research method
Surface wave dispersion curve method
Tangential energy minimum method
Silver & Chan, 1991, JGR
Chevrot, 2000, JGR