P- and S-wave velocity of dry, water-saturated, and frozen basalt: Implications for the interpretation of Martian seismic data

The theoretical predictions for the P- and S-wave velocity of basalt with pore spaces filled with gaseous CO2, liquid water, or water ice presented herein could help improve interpretations of the seismic data collected by NASA's InSight lander, which landed on the Martian surface in November 2018.