000008206 001__ 8206
000008206 005__ 20261014152137.0
000008206 0247_ $$2DOI$$a10.1016/j.icarus.2026.117148
000008206 037__ $$aSCART-2026-0161
000008206 100__ $$aSamuel, Henri
000008206 245__ $$aComplementary analyses further support a molten Basal Mantle Layer on Mars: A reply to Russell et al. (2026)
000008206 260__ $$c2026
000008206 520__ $$aSeismic data offer a unique window into planetary interiors. Here, following a note from Russell et al. (2026), we provide further analysis to solidify our identification of a seismic phase detected by the InSight mission as one which interacts with a basal mantle layer (BML) on Mars (Samuel et al., 2023a). We show that other mantle discontinuities or other seismic structures invoked in the aforementioned note are unlikely to produce this seismic signal. We further illustrate how our proposed layered structure is compatible with other available geophysical observations and geodynamical constraints, and can be used to make inferences about Martian evolution.
000008206 536__ $$a3PRODPLANINT/$$c3PRODPLANINT/$$f3PRODPLANINT
000008206 594__ $$aNO
000008206 700__ $$aDrilleau, Mélanie
000008206 700__ $$aLekić, Vedran
000008206 700__ $$aIrving, Jessica C. E.
000008206 700__ $$aXu, Zongbo
000008206 700__ $$aHuang, Quancheng
000008206 700__ $$aGarcia, Raphaël F.
000008206 700__ $$aRivoldini, Attilio
000008206 700__ $$aBadro, James
000008206 700__ $$aLognonné, Philippe H.
000008206 700__ $$aConnolly, James A. D.
000008206 700__ $$aKawamura, Taichi
000008206 700__ $$aGudkova, Tamara
000008206 700__ $$aBanerdt, William B.
000008206 773__ $$pICARUS$$v458$$y2026
000008206 8560_ $$fattilio.rivoldini@ksb-orb.be
000008206 8564_ $$s4559255$$uhttps://publi2-as.oma.be/record/8206/files/Samuel2026aa00.pdf
000008206 8564_ $$s5079$$uhttps://publi2-as.oma.be/record/8206/files/Samuel2026aa00.gif?subformat=icon$$xicon
000008206 8564_ $$s7971$$uhttps://publi2-as.oma.be/record/8206/files/Samuel2026aa00.jpg?subformat=icon-180$$xicon-180
000008206 905__ $$apublished in
000008206 980__ $$aREFERD