Published March 31, 2023 | Version v1

Velocity models from "Investigation of Martian regional crustal structure near the dichotomy using S1222a surface-wave group velocities"

Description

The isotropic velocity models from joint inversion of Rayleigh- and Love-wave group-velocity measurements of S1222a. The details about these models and the joint inversion are in "Investigation of Martian regional crustal structure near the dichotomy using S1222a surface-wave group velocities" which is submitted to GRL.

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Additional details

Funding

Agence Nationale de la Recherche
MAGIS - MArs Geophysical InSight ANR-19-CE31-0008