المؤلفون: Carrasco, S., Knapmeyer-Endrun, Brigitte, Margerin, L., Xu, Z., Joshi, R., Schimmel, Martin, Stutzmann, Eleonore, Charalambous, C., Lognonné, P., Banerdt, W. B.

مصطلحات موضوعية: Rayleigh waves ellipticity was measured between periods 15–35 s at the InSight landing site using large seismic events, including S1222a, A 4-layer crust, including a shallow low-velocity layer, is required to explain the ellipticity, receiver functions and P-wave lag times, Low crustal velocities are derived for the InSight site, which may be due to high porosity or heavy alteration at local scale

Relation: http://dx.doi.org/10.1029/2023GL104816; Sí; Geophysical Research Letters, 50(16): e2023GL104816 (2023); http://hdl.handle.net/10261/347851

الاتاحة: http://hdl.handle.net/10261/347851
https://doi.org/10.1029/2023GL104816