
Mercury
Mercury’s Magma Ocean May Have Built Its Layered Mantle
Laboratory experiments and numerical modeling suggest that Mercury’s sulfur-rich primordial magma ocean crystallized into a strongly layered mantle, with its deepest structure depending on the planet’s original magnesium-to-silicon ratio. The study finds that a shallower, clinopyroxene-bearing fertile mantle could have supplied enough partial melt to build much of Mercury’s volcanic crust, while sulfur may have driven dense sulfides into the mantle and altered the distribution of heat-producing elements.















