Hollow-Forming Layers in Impact Craters on Mercury: Massive Sulfide or Chloride Deposits Formed by Impact Melt Differentiation?

Details Hollow-Forming Layers in Impact Craters on Mercury: Massive Sulfide or Chloride Deposits Formed by Impact Melt Differentiation? Hollow-Forming Layers in Impact Craters on Mercury: Massive Sulfide or Chloride Deposits Formed by Impact Melt Differentiation?

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1187v&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1187

Physics

Scientific paper

We map the geology of the heavily hollowed crater Kertesz and show that
hollows in this crater develop in a 30-meter-thick hollow-forming layer
derived from impact melt. This layer may be a massive sulfide or
chloride impact melt differentiate.

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