Flow and fabric deep down

Karen M. Fischer ()
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Karen M. Fischer: Brown University

Nature, 2002, vol. 415, issue 6873, 745-747

Abstract: Conditions in Earth's mantle can be inferred from seismic-wave velocities which reveal areas of anisotropy. Evidence emerges of such an area at mid-mantle level, associated with a subducting tectonic plate.

Date: 2002
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DOI: 10.1038/415745a

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