Viscosity of peridotite liquid up to 13 GPa: Implications for magma ocean viscosities

By C. Liebske, B. Schmickler, H. Terasaki, B. Poe, A. Suzuki, K. Funakoshi, R. Ando, D. Rubie. 2005

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Linked magma ocean solidification and atmospheric growth for Earth and Mars (2008, background): “At expected magma ocean viscosities of 0.1 to 1 Pa s (Liebske et al., 2005), the settling vs. entrainment expression of Solomatov et al. (1993) predicts that grains must be less than a millimeter in diameter to remain entrained in flow; those larger will settle or rise.”
Emergence of a Habitable Planet (2007, background): “Viscosity varies by at least 15 orders of magnitude over a small temperature range when near the solidus (Liebske et al. 2005).”