Magmatic and impact-induced gas-solid reactions controlled the early evolution of the martian surface and atmosphere
Penelope Lineton King1, Richard W Henley2, Hanna Nekvasil3, John Moores4, Christian Renggli1,5, Andrew B. Palm1, Jeff Berger6, Vadim S Kamenetsky7 and Pierre Delmelle8, (1)Australian National University, Research School of Earth Sciences, Canberra, ACT, Australia, (2)Australian National University, Research School of Physics & Engineering, Canberra, ACT, Australia, (3)Stony Brook University, Geosciences, Stony Brook, NY, United States, (4)York University, Toronto, ON, Canada, (5)University of Münster, Institute for Mineralogy, Münster, Germany, (6)NASA JSC, Houston, TX, United States, (7)University of Tasmania, CODES, Hobart, Australia, (8)Université Catholique de Louvain, Louvain-La-Neuve, Belgium