Thermochemical evolution of Mercury's interior
By Nicola Tosi, Matthias Grott, A. Plesa, Doris Breuer. 2013
142 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/d1578d02962acc74a5398affa9e488d8a08011d6
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In Astronomy and Astrophysics
- Denton S. Ebel
- Sean C. Solomon
- S. Hauck,
- James W. Head III
- L. Nittler
- R. Wordsworth
- Mark A. Wieczorek
- Maria T. Zuber
In Atmospheric Science
Citations in the corpus
- Evidence for geochemical terranes on Mercury: Global mapping of major elements with MESSENGER's X-Ray Spectrometer (2015, background): “Given the shallow depth of Mercury’s core–mantle boundary (Smith et al., 2012; Hauck et al., 2013), it is possible that mantle convection was not vigorous throughout the planet’s evolution (Michel et al., 2013; Tosi et al., 2013) and therefore the mantle did not become well homogenized.”