A seismic model of the lunar mantle and constraints on temperature and mineralogy
By J. Gagnepain-Beyneix, Philippe Lognonné, Hugues Chenet, D. Lombardi, Tilman Spohn. 2006
158 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Geophysics
View Paper: https://www.semanticscholar.org/paper/26fe1216592cb891520b8dc0263a124d56468c68
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In Astronomy and Astrophysics
In Geophysics
Citations in the corpus
- Crystallization of the lunar magma ocean and the primordial mantle-crust differentiation of the Moon (2018, background): “However, a broad range of acceptable models has been proposed and caution should be taken with the interpretation of that seismic discontinuity (Gagnepain-Beyneix et al., 2006; Wieczorek et al., 2006; Lognonné and Johnson, 2007; Khan et al., 2013).”
- A 3‐D numerical study of the thermal evolution of the Moon after cumulate mantle overturn: The importance of rheology and core solidification (2013, result): “These predictions are generally consistent with the deepmantle temperatures suggested from seismic and gravitational inversions (Figure 9) [e.g., Khan et al., 2006; Gagnepain-Beyneix et al., 2006; Frohlich and Nakamura, 2009], and electrical conductivity study [Hood et al.”