The Mg-carbonate–Fe interaction: Implication for the fate of subducted carbonates and formation of diamond in the lower mantle
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DOI: 10.1016/j.gsf.2018.10.003
Abstract: Abstract The fate of subducted carbonates in the lower mantle and at the core-mantle boundary was modelled via experiments in the MgCO3-Fe0 system at 70–150 GPa and 800–2600 K in a laser-heated diamond anvil cell. Using in… read more here.
Keywords: lower mantle; interaction; fate subducted; subducted carbonates ... See more keywords