The Importance of a High Viscosity Peak at 2000 km Depth for Time-Dependent Convection Dynamics: An Explanation for the Dominance of Degree-2 Structure in the Lower-most Mantle.

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ADS bibcode: 2001AGUFM.T51D..01F
year: 2001
Listed Authors: Forte, A. M.; Espesset, A.
Listed Institutions: University of Western Ontario, Department of Earth Sciences, Biology and Geology Building, London, ON N6A 5B7 Canada; University of Western Ontario, Department of Earth Sciences, Biology and Geology Building, London, ON N6A 5B7 Canada

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University of Western Ontario, Canada