Anistropy in the Inner Core: Could It Be Due To Low-Order Convection?

Details Anistropy in the Inner Core: Could It Be Due To Low-Order Convection? Anistropy in the Inner Core: Could It Be Due To Low-Order Convection?

Nov 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996sci...274..963r&link_type=abstract

Science, Volume 274, Issue 5289, pp. 963-966

Computer Science

31

Scientific paper

A recently assembled data set of inner core-sensitive free oscillation splitting measurements and body wave differential travel times provides constraints on the patterns of anisotropy in the Earth's inner core. Applying a formalism that allows departures from radial symmetry and cylindrical anisotropy results in models with P-wave velocity distributions whose strength and pattern are incompatible with frozen-in anisotropy, but rather suggest a simple large-scale convection regime in the inner core.

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