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Christopher Davies
University of LeedsMeeting roles in:
Inertia-Corrected Equatorial Core-Mantle-Boundary Heat Flux Heterogeneities are correlated with reversal rates from 200 Ma
Using Legendre Polynomial Based Paleosecular Variation Models to Infer Dynamo Dipolarity
Effect of a Chemically Stratified F-layer in Rotating Spherical Shell Convection
Thermochemical geodynamos with heterogeneous core-mantle boundary heat flux
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