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- Shear_wave_splitting abstract "Shear wave splitting, also called seismic birefringence, is the phenomenon that occurs when a polarized shear wave enters an anisotropic medium (Fig. 1). The incident shear wave splits into two polarized shear waves (Fig. 2). Shear wave splitting is typically used as a tool for testing the anisotropy of an area of interest. These measurements reflect the degree of anisotropy and lead to a better understanding of the area’s crack density and orientation or crystal alignment. We can think of the anisotropy of a particular area as a black box and the shear wave splitting measurements as a way of looking at what is in the box.".
- Shear_wave_splitting thumbnail Erin_Isotropic_anisotropic.png?width=300.
- Shear_wave_splitting wikiPageExternalLink garnero15ani_crampin3.jpg.
- Shear_wave_splitting wikiPageExternalLink garnero_splitting.gif.
- Shear_wave_splitting wikiPageExternalLink index.html.
- Shear_wave_splitting wikiPageExternalLink shear_wave_splitting.
- Shear_wave_splitting wikiPageExternalLink character.html.
- Shear_wave_splitting wikiPageExternalLink splitting.
- Shear_wave_splitting wikiPageExternalLink 27548.
- Shear_wave_splitting wikiPageID "27310834".
- Shear_wave_splitting wikiPageRevisionID "602476598".
- Shear_wave_splitting hasPhotoCollection Shear_wave_splitting.
- Shear_wave_splitting subject Category:Earthquakes.
- Shear_wave_splitting subject Category:Seismological_observatories.
- Shear_wave_splitting subject Category:Seismology.
- Shear_wave_splitting type Artifact100021939.
- Shear_wave_splitting type Building102913152.
- Shear_wave_splitting type Object100002684.
- Shear_wave_splitting type Observatory103839671.
- Shear_wave_splitting type PhysicalEntity100001930.
- Shear_wave_splitting type SeismologicalObservatories.
- Shear_wave_splitting type Structure104341686.
- Shear_wave_splitting type Whole100003553.
- Shear_wave_splitting type YagoGeoEntity.
- Shear_wave_splitting type YagoPermanentlyLocatedEntity.
- Shear_wave_splitting comment "Shear wave splitting, also called seismic birefringence, is the phenomenon that occurs when a polarized shear wave enters an anisotropic medium (Fig. 1). The incident shear wave splits into two polarized shear waves (Fig. 2). Shear wave splitting is typically used as a tool for testing the anisotropy of an area of interest. These measurements reflect the degree of anisotropy and lead to a better understanding of the area’s crack density and orientation or crystal alignment.".
- Shear_wave_splitting label "Shear wave splitting".
- Shear_wave_splitting sameAs m.0bx_gfv.
- Shear_wave_splitting sameAs Q7492182.
- Shear_wave_splitting sameAs Q7492182.
- Shear_wave_splitting sameAs Shear_wave_splitting.
- Shear_wave_splitting wasDerivedFrom Shear_wave_splitting?oldid=602476598.
- Shear_wave_splitting depiction Erin_Isotropic_anisotropic.png.
- Shear_wave_splitting isPrimaryTopicOf Shear_wave_splitting.
