Thickness of the crust of Mercury from geoid‐to‐topography ratios

@article{Padovan2015ThicknessOT,
  title={Thickness of the crust of Mercury from geoid‐to‐topography ratios},
  author={Sebastiano Padovan and Mark A. Wieczorek and Jean-Luc Margot and Nicola Tosi and Sean C. Solomon},
  journal={Geophysical Research Letters},
  year={2015},
  volume={42},
  pages={1029 - 1038}
}
To gain insight into the thickness of the crust of Mercury, we use gravity and topography data acquired by the MErcury Surface, Space ENvironment, GEochemistry, and Ranging spacecraft to calculate geoid‐to‐topography ratios over the northern hemisphere of the planet. For an Airy model for isostatic compensation of variations in topography, we infer an average crustal thickness of 35 ± 18 km. Combined with the value of the radius of the core of Mercury, this crustal thickness implies that… 
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