How can seismology help to learn about Mars interior. This is a short presentation that was originally made for the fall meeting of the American Geophysical Union. Please excuse the poor video quality.
The content is collected from the following scientific papers:
Banerdt, W.B., Smrekar, S.E., et al., 2020. Initial results from the InSight mission on Mars. Nature Geoscience 13, 183–189. https://doi.org/10.1038/s41561-020-05...
Clinton, J.F., Ceylan, S., et al., 2021. The Marsquake catalogue from InSight, sols 0–478. Physics of the Earth and Planetary Interiors 310. https://doi.org/10.1016/j.pepi.2020.1...
Giardini, D., Lognonné, P., et al., 2020. The seismicity of Mars. Nat. Geosci. 13, 205–212. https://doi.org/10.1038/s41561-020-05...
Karakostas, F., Schmerr, N., et al., 2021. Scattering Attenuation of the Martian Interior through Coda‐Wave Analysis. Bulletin of the Seismological Society of America. https://doi.org/10.1785/0120210253
Khan, A., Ceylan, S., et al., 2021. Imaging the upper mantle structure of Mars with InSight seismic data. Science 373, 434–438.
Knapmeyer-Endrun, B., Panning, M.P., et al., 2021. Thickness and structure of the martian crust from InSight seismic data. Science 373, 438–443. https://doi.org/10.1126/science.abf8966
Lognonné, P., Banerdt, W.B., et al., 2020. Constraints on the shallow elastic and anelastic structure of Mars from InSight seismic data. Nature Geoscience 13, 213–220. https://doi.org/10.1038/s41561-020-05...
Menina, S., Margerin, L., et al., 2021. Energy Envelope and Attenuation Characteristics of High‐Frequency (HF) and Very‐High‐Frequency (VF) Martian Events. Bulletin of the Seismological Society of America. https://doi.org/10.1785/0120210127
Stähler, S.C., Khan, A., et al., 2021. Seismic detection of the martian core. Science 373, 443–448. https://doi.org/10.1126/science.abi7730
van Driel, M., Ceylan, S., et al., 2021. High-Frequency Seismic Events on Mars Observed by InSight. Journal of Geophysical Research: Planets 126, e2020JE006670. https://doi.org/10.1029/2020JE006670
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