• Seismic Velocity Variations in a 3D Martian Mantle: Implications for the InSight Measurements 

      Plesa, A.‐C.ORCIDiD; Bozdağ, E.ORCIDiD; Rivoldini, A.ORCIDiD; Knapmeyer, M.ORCIDiD; McLennan, S. M.ORCIDiD; Padovan, S.ORCIDiD; Tosi, N.ORCIDiD; Breuer, D.ORCIDiD; Peter, D.ORCIDiD; Stähler, S.ORCIDiD; Wieczorek, M. A.ORCIDiD; van Driel, M.ORCIDiD; Khan, A.ORCIDiD; Spohn, T.ORCIDiD (Journal of Geophysical Research: Planets, 2021-06-17)
      We use a large data set of 3D thermal evolution models to predict the distribution of present‐day seismic velocities in the Martian interior. Our models show a difference between maximum and minimum S wave velocity of up ...
    • The Global Seismic Moment Rate of Mars After Event S1222a 

      Knapmeyer, M.ORCIDiD; Stähler, S.ORCIDiD; Plesa, A.‐C.ORCIDiD; Ceylan, S.ORCIDiD; Charalambous, C.ORCIDiD; Clinton, J.; Dahmen, N.ORCIDiD; Durán, C.; Horleston, A.ORCIDiD; Kawamura, T.ORCIDiD; Kim, D.; Li, J.; Plasman, M.; Zenhäusern, G.ORCIDiD; Weber, R. C.ORCIDiD; Giardini, D.ORCIDiD; Panning, M. P.ORCIDiD; Lognonné, P.ORCIDiD; Banerdt, W. B.ORCIDiD (Geophysical Research Letters, 2023-04-06)
      The seismic activity of a planet can be described by the corner magnitude, events larger than which are extremely unlikely, and the seismic moment rate, the long‐term average of annual seismic moment release. Marsquake ...