Geodesy constraints on the interior structure and composition of Mars
By A. Rivoldini, T. Hoolst, O. Verhoeven, A. Mocquet, Véronique Dehant. 2011
223 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/16b4f0de15ff2d2945341353b3fb2d9bf5e107fc
How researchers see this paper
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In Astronomy and Astrophysics
- Mark A. Wieczorek
- F. Nimmo
- Y. Alibert
- W. Benz
- Amir Khan
- Philippe Lognonné
- T. O. S. University
- Research School of Earth Sciences
In Molecular Biology
- F. Nimmo
- Paul J. Tackley
- J. A. Connolly
- Philippe Lognonné
- Mark A. Wieczorek
- U. Christensen
- Julien Aubert
- Johannes Wicht
Citations in the corpus
- Can we constrain the interior structure of rocky exoplanets from mass and radius measurements (2015, result): “Comparing our results to models with pure iron cores (Rivoldini et al. 2011; Khan & Connolly 2008), reduces discrepancy.”
- The seismicity of Mars (2020, methodology): “The latter was composed of an adiabatic liquid iron alloy core (with the light element assumed to be sulfur, see Rivoldini et al. (2011), surrounded by a silicate envelope.”
- The composition of Mars (2019, result): “, 2016) and FeO (Lee and Gaskell, 1974; Komabayashi, 2014) and solid FeH (Umemoto and Hirose, 2015) at core pressures and temperatures and a third-order finite strain Birch-Murnaghan or Vinet equation of state (Stixrude and Lithgow-Bertelloni, 2005), following previous studies (Longhi et al., 1992; ”