Three-dimensional localized Rayleigh–Bénard convection in temperature-dependent viscosity fluids von Solomatov, V. S.

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Scaling of time-dependent stagnant lid convection: Application to small-scale convection on Earth and other terrestrial planets von Solomatov, V. S., Moresi, L.‐N.

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Initiation of subduction by small-scale convection von Solomatov, V. S.

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Grain size variations in the Earth's mantle and the evolution of primordial chemical heterogeneities von Solomatov, V. S., Reese, C. C.

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Onset of convection in internally heated fluids with strongly temperature-dependent viscosity von Jain, C., Solomatov, V. S.

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Fluid dynamics of local martian magma oceans von Reese, C.C., Solomatov, V.S.

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Stability range of localized subcritical Rayleigh–Bénard convection in temperature-dependent viscosity fluids: Constraints from two-dimensional simulations von Solomatov, V. S., Jain, C.

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Impact origin for the Martian crustal dichotomy: Half emptied or half filled? von Reese, C. C., Orth, C. P., Solomatov, V. S.

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Early martian dynamo generation due to giant impacts von Reese, C.C., Solomatov, V.S.

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Early transient superplumes and the origin of the Martian crustal dichotomy von Ke, Y., Solomatov, V. S.

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Impact megadomes and the origin of the martian crustal dichotomy von Reese, C.C., Orth, C.P., Solomatov, V.S.

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Analysis of the Cessation of Convection in Mercury's Mantle von Jain, C., Solomatov, V. S.

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Magmatic evolution of impact-induced Martian mantle plumes and the origin of Tharsis von Reese, C. C., Solomatov, V. S., Baumgardner, J. R., Stegman, D. R., Vezolainen, A. V.

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Heat transport efficiency for stagnant lid convection with dislocation viscosity: Application to Mars and Venus von Reese, C. C., Solomatov, V. S., Moresi, L.‐N.

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Scaling of temperature‐ and stress‐dependent viscosity convection von Solomatov, V. S.

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Coupled core-mantle thermal evolution of early Mars von Ke, Y., Solomatov, V. S.

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Three regimes of mantle convection with non-Newtonian viscosity and stagnant lid convection on the terrestrial planets von Solomatov, V. S., Moresi, L.-N.

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Can hotter mantle have a larger viscosity? von Solomatov, V. S.

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The isostatic stagnant lid approximation and global variations in the Venusian lithospheric thickness von Orth, C. P., Solomatov, V. S.

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Constraints on the Venusian crustal thickness variations in the isostatic stagnant lid approximation von Orth, C. P., Solomatov, V. S.

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