Redox freezing and melting in the Earth’s deep mantle resulting from carbon–iron redox coupling

Carbon speciation in the asthenosphere: Experimental measurements of the redox conditions at which carbonate-bearing melts coexist with graphite or diamond in peridotite assemblages

(2010) Vincenzo Stagno et al.   EARTH AND PLANETARY SCIENCE LETTERS

The deep carbon cycle and melting in Earth's interior

(2010) Rajdeep Dasgupta et al.   EARTH AND PLANETARY SCIENCE LETTERS

Solidus of carbonated peridotite from 10 to 20 GPa and origin of magnesiocarbonatite melt in the Earth's deep mantle

(2009) Sujoy Ghosh et al.   CHEMICAL GEOLOGY

High pressure effects on the iron–iron oxide and nickel–nickel oxide oxygen fugacity buffers

(2009) Andrew J. Campbell et al.   EARTH AND PLANETARY SCIENCE LETTERS

Melting in the Fe–C system to 70 GPa

(2009) O.T. Lord et al.   EARTH AND PLANETARY SCIENCE LETTERS

Centrifuge assisted percolation of Fe–S melts in partially molten peridotite: Time constraints for planetary core formation

(2009) N. Bagdassarov et al.   EARTH AND PLANETARY SCIENCE LETTERS

Permeability of asthenospheric mantle and melt extraction rates at mid-ocean ridges

(2009) James A. D. Connolly et al.   NATURE

Solidus and phase relations of carbonated peridotite in the system CaO–Al2O3–MgO–SiO2–Na2O–CO2 to the lower mantle depths

(2009) Konstantin D. Litasov et al.   PHYSICS OF THE EARTH AND PLANETARY INTERIORS

The Redox State of Earth's Mantle

(2008) Daniel J. Frost et al.   Annual Review of Earth and Planetary Sciences