Abstract: Carbonation of Subduction Interface Ultramafic Rocks and Implications for Deep Carbon Cycling: Evidence from Hybrid Serpentinite-Marble in the Voltri Massif, Italy (2015 AGU Fall Meeting)

Carbonation of Subduction Interface Ultramafic Rocks and Implications for Deep Carbon Cycling: Evidence from Hybrid Serpentinite-Marble in the Voltri Massif, Italy

Marco Scambelluri¹, Gray E Bebout², Mattia Gilio¹, Donato Belmonte¹, Nicola Campomenosi¹ and Laura Crispini³, (1)University of Genoa, Genoa, Italy, (2)Lehigh University, Dept. Earth and Environmental Sciences, Bethlehem, PA, United States, (3)University of Genova, Department of Earth Sciences, Environment and Life, Genova, Italy

Back to: The Earth's Geodynamic Carbon Cycle: Subduction, Storage, Migration, and Outgassing I