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Investigation of Venus’ Thermal History, Crustal Evolution, and Core Dynamics with a Coupled Interior-lithosphere-atmosphere Model

  • Authors: Rodolfo Garcia, Rory Barnes, Peter E. Driscoll, Victoria S. Meadows, Megan Gialluca

Rodolfo Garcia et al 2026 The Planetary Science Journal 7 .

  • Provider: AAS Journals

Caption: Figure 16.

Evolution of key mantle parameters for a Type I evolution (black) and a Type II evolution (blue). Venus’ age is demarcated with a dashed vertical black line. Note that after about 5.5 Gyr, the Type I evolution begins to exhibit Type II–like behavior (a ramp-up in viscosity, a ramp-down to 0 in the upper melt fraction, and a subsequent total loss of water in the atmosphere). Parameter choices for these evolutions can be found in Table 8.

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