The buffering capacity of lithospheric mantle: implications for diamond formation

2014/11/01 by Robert W. Luth, Thomas Stachel · 8 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #High-pressure geophysics and materials #earthquake and tectonic studies

paper · doi:10.1007/s00410-014-1083-6

Citations

• The composition of the Earth
• The garnet-clinopyroxene Fe-Mg geothermometer ? a reinterpretation of existing experimental data

Cited by

• High-pressure phase relations in the Mg–Fe–O system and the conditions at which ferropericlase inclusions in diamonds are formed
• Archaean and Proterozoic diamond growth from contrasting styles of large-scale magmatism. [europepmc]
• Ti 3+ in corundum traces crystal growth in a highly reduced magma. [europepmc]
• Oxidation state and metasomatism of the lithospheric mantle beneath the Rae Craton, Canada: strong gradients reflect craton formation and evolution. [europepmc]
• Insights on the deep carbon cycle from the electrical conductivity of carbon-bearing aqueous fluids. [europepmc]
• Evidence for oxygen-conserving diamond formation in redox-buffered subducted oceanic crust sampled as eclogite. [europepmc]
• Deep carbon cycling during subduction revealed by coexisting diamond-methane-magnesite in peridotite. [europepmc]
• Trace element systematics constrain the origin of fluids that form gem-quality diamonds. [europepmc]