Comments on “Using the viscoelastic relaxation of large impact craters to study the thermal history of Mars” (Karimi et al., 2016, Icarus 272, 102–113) and “Studying lower crustal flow beneath mead basin: Implications for the thermal history and rheology of Venus” (Karimi and Dombard, 2017, Icarus 282, 34–39)

1. Ruiz, J.
2. Jiménez-Díaz, A.
3. Egea-González, I.
4. Parro, L.M.
5. Mansilla, F.