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About: Shear wave splitting     Goto   Sponge   NotDistinct   Permalink

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Type: yago:WikicatSeismologicalObservatoriesyago:Artifact100021939yago:Building102913152yago:Object100002684yago:Observatory103839671yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntitydiseaseyago:Structure104341686yago:Whole100003553 New Facet based on Instances of this Class

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.