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Seismic anisotropy: tracing plate dynamics in the mantle

Jeffrey Park1, Vadim Levin

  • 1Department of Geology and Geophysics, Yale University, Post Office Box 208109, New Haven, CT 06520-8109, USA.

Science (New York, N.Y.)
|April 20, 2002
PubMed
Summary

Elastic anisotropy, where seismic wave speed varies by direction, is key to understanding Earth's mantle and crust. This phenomenon, driven by mineral orientation, aids geophysicists in exploring rock textures and mantle dynamics.

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