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The role of edge-driven convection in the generation ofvolcanism – Part 2: Interaction with mantle plumes, applied to the Canary Islands 由 A. Manjón-Cabeza Córdoba, A. Manjón-Cabeza Córdoba, A. Manjón-Cabeza Córdoba, M. D. Ballmer, M. D. Ballmer

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Narrow, Fast, and “Cool” Mantle Plumes Caused by Strain‐Weakening Rheology in Earth's Lower Mantle 由 A. J. P. Gülcher, G. J. Golabek, M. Thielmann, M. D. Ballmer, P. J. Tackley

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Plume–ridge interactions: ridgeward versus plate-drag plume flow 由 F. Pang, J. Liao, J. Liao, J. Liao, M. D. Ballmer, L. Li, L. Li, L. Li

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