All abstracts by Megan S. Duncan in conference series: Goldschmidt
(2017) Limited Dissolution of Organic Carbon in Slab Melt Causes the Rise of Atmospheric O2 Across GOEDasgupta R & Duncan MS
(2015) Origin and Evolution of C-O-H Volatiles in Terrestrial Magma Ocean, Earth’s Hadean Mantle, and Atmosphere
Dasgupta R, Li Y & Duncan MS
(2013) Solubility of CO2 in Rhyolitic Melts as a Function of Depth, Temperature, and Oxygen Fugacity – Implications for Carbon Flux in Subduction Zones
Duncan M & Dasgupta R
(2013) Deep Subduction of Carbon and Sulfur Constrained by Laboratory Experiments
Dasgupta R, Duncan M, Jégo S & Tsuno K