Abstract: Elevated Zinc and Germanium Discovered by <i>Curiosity’s</i> APXS in the Murray Formation of Gale Crater, Mars, Indicate Hydrothermal Enrichment and Possible Diagenetic Fractionation (2017 AGU Fall Meeting)

Elevated Zinc and Germanium Discovered by Curiosity’s APXS in the Murray Formation of Gale Crater, Mars, Indicate Hydrothermal Enrichment and Possible Diagenetic Fractionation

Jeff A. Berger¹, Ralf Gellert², Mariek E Schmidt³, Nicholas Boyd², Elstan Desouza², Douglas W Ming⁴, Catherine O'Connell-Cooper⁵, Elizabeth B Rampe⁴, Lucy M Thompson⁵, Scott VanBommel⁶ and Albert Yen⁷, (1)University of Guelph, Department of Physics, Guelph, ON, Canada, (2)University of Guelph, Guelph, ON, Canada, (3)Brock University, St Catharines, ON, Canada, (4)NASA Johnson Space Center, Houston, TX, United States, (5)University of New Brunswick, Fredericton, NB, Canada, (6)University of Guelph, Guelph, Canada, (7)NASA Jet Propulsion Laboratory, Pasadena, CA, United States

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