Title: Mineral Monday: Mercury, the Sulfur rich planet by Emily Fischer
MESSENGER X-Ray Spectrometer (XRS) surface composition maps of Mercury (from Nittler et al., 2020, Icarus). Si is estimated at ~25 wt%. The spatial correlation between Mg and S is consistent with the presence of Mg-bearing sulfides such as niningerite (MgS) at the surface.
BSE image of a high-temperature, low-pressure experimental run product from Namur et al. (2016, EPSL) showing FeS and mixed Mg-Ca-Fe sulfide phases, analogues for the exotic sulfide mineralogy expected on Mercury's surface.
Hollows on Mercury's surface and proposed formation stages (from Deutsch et al. 2025, JGR Planets). These rimless depressions are unique in the solar system These minerals may also be behind one of Mercury’s strangest features: hollows. These bizarre, rimless depressions are unique to Mercury and are still forming today! The leading idea is that sulfide minerals destabilize under Mercury’s extreme surface conditions and essentially sublimate away, leaving shallow pits behind.
Mineral Monday by Emily Fischer
Mercury is one of the most chemically reduced bodies in the solar system, meaning very little free oxygen. It likely hosts a wild suite of sulfide minerals: oldhamite (CaS) and niningerite (MgS), and potentially exotic Na- and K-bearing sulfides.
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