# data[].attributes.body
left= magnesium/silicate.right=aluminium silicate

https://www.nasa.gov/image-feature/showing-some-chemistry

# data[].attributes.body
mostly silicate materials including aluminum silicate and magnesium silicate. less than 6% weight of surface material is solar from the core.

http://science.sciencemag.org/content/321/5885/59

https://www.sciencedirect.com/science/article/pii/S001910350800448X

# data[].attributes.body
Iron rich with 5% sulfur in the inner core and 10% at the mantle boundary

# data[].attributes.body
The four key events in the origin hypothesis of
Mercury. (A) Global melting of the planet and separation
of a metallic core from a silicate magma ocean. (B) Cooling of
the planet, progressive crystallization of the solid inner core, potential
formation of an FeS layer at the core–mantle boundary, and
crystallization of the magma ocean to produce the primordial
mantle and a graphite flotation crust.
(C) Partial melting of the
mantle, production of the secondary crust, and synchronous
cratering of the surface.
(D) Termination of major volcanism at
about 3.6 Ga and global planetary contraction

Bernard Charlier, Olivier Namur; The Origin and Differentiation of Planet Mercury. Elements ; 15 (1): 9–14. doi: https://doi.org/10.2138/gselements.15.1.9

# data[].attributes.body
Figure 1. Mercury's interior structure compared to that of the Earth (from Stevenson et al., 2012).