Solidus and liquidus profiles of chondritic mantle: Implication for melting of the Earth across its history
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April 2011 |
Melting of subducted basalt at the core-mantle boundary
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May 2014 |
Diamond nucleation and growth by reduction of carbonate melts under high-pressure and high-temperature conditions
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January 2002 |
Diamond formation from CaCO3 at high pressure and temperature [Diamond formation from CaCO3 at high pressure and temperature]
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March 2010 |
Experimental evidence for carbonate stability in the Earth's lower mantle
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July 1993 |
New host for carbon in the deep Earth
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March 2011 |
Experimental investigation of the stability of Fe-rich carbonates in the lower mantle: STABILITY OF CARBONATES IN THE MANTLE
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February 2012 |
Carbonates from the lower part of transition zone or even the lower mantle
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August 2007 |
Thermodynamic parameters in the Earth as determined from seismic profiles
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September 1981 |
Measurement of temperature distributions across laser heated samples by multispectral imaging radiometry
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January 2008 |
Redox Heterogeneity in Mid-Ocean Ridge Basalts as a Function of Mantle Source
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May 2013 |
The deep carbon cycle and melting in Earth's interior
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September 2010 |
Spin transition and equations of state of (Mg, Fe)O solid solutions
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January 2007 |
Equation of state and phase diagram of FeO
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April 2011 |
Experimental evidence for the existence of iron-rich metal in the Earth's lower mantle
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March 2004 |
The Redox State of Earth's Mantle
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May 2008 |
Phase relations and melting of carbonated peridotite between 10 and 20 GPa: a proxy for alkali- and CO2-rich silicate melts in the deep mantle
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February 2014 |
Diamond formation in the deep mantle: the record of mineral inclusions and their distribution in relation to mantle dehydration zones
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April 2010 |
Nucleation and growth of diamond using NiTi, NiNb and FeB alloy as solvents
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January 1996 |
Stability of magnesite and its high-pressure form in the lowermost mantle
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January 2004 |
Mineralogy of the lower mantle: A review of ‘super-deep’ mineral inclusions in diamond
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January 2012 |
A primary natrocarbonatitic association in the Deep Earth
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February 2015 |
Melting and subsolidus phase relations in the MgSiO3MgCO3 system at high pressures: implications to evolution of the Earth's atmosphere
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July 1990 |
Reevaluating carbon fluxes in subduction zones, what goes down, mostly comes up
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June 2015 |
Finite element simulations of the laser-heated diamond-anvil cell
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June 2005 |
Simulating the core-mantle boundary: An experimental study of high-pressure reactions between silicates and liquid iron
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July 1989 |
Vibrational and elastic properties of ferromagnesite across the electronic spin-pairing transition of iron
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March 2012 |
Static compression of iron to 300 GPa and Fe 0.8 Ni 0.2 alloy to 260 GPa: Implications for composition of the core
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January 1990 |
Role of iron and reducing conditions on the stability of dolomite + coesite between 4.25 and 6 GPa a potential mechanism for diamond formation during subduction [Role of iron and reducing conditions on the stability of dolomite + coesite between 4.25 and 6 GPa a potential mechanism for diamond formation during subduction]
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February 2011 |
Experimental investigation of silicate-carbonate system at high pressure and high temperature
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March 1998 |
The reactions between iron and magnesite at 6 GPa and 1273–1873 K: Implication to reduction of subducted carbonate in the deep mantle
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January 2015 |
Reactions of iron with calcium carbonate at 6 GPa and 1273–1873 K: implications for carbonate reduction in the deep mantle
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September 2015 |
The CaCO3–Fe interaction: Kinetic approach for carbonate subduction to the deep Earth’s mantle
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October 2016 |
Mineral Inclusions in Diamonds from the Sloan Kimberlites, Colorado
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July 1986 |
Low Core-Mantle Boundary Temperature Inferred from the Solidus of Pyrolite
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January 2014 |
Novel high-pressure structures of MgCO3, CaCO3 and CO2 and their role in Earth's lower mantle
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August 2008 |
High-pressure transition of CaCO3
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July 2007 |
Post-aragonite phase transformation in CaCO3 at 40 GPa
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April 2005 |
Deep penetration of molten iron into the mantle caused by a morphological instability
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December 2012 |
Mantle-slab interaction and redox mechanism of diamond formation
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December 2013 |
Diamond formation through carbonate-silicate interaction
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July 2002 |
Diamond formation from mantle carbonate fluids
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July 1999 |
Structures and stability of calcium and magnesium carbonates at mantle pressures
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March 2015 |
Advanced flat top laser heating system for high pressure research at GSECARS: application to the melting behavior of germanium
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September 2008 |
Temperature distributions in the laser-heated diamond anvil cell from 3-D numerical modeling
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November 2013 |
Metal saturation in the upper mantle
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September 2007 |
Redox freezing and melting in the Earth’s deep mantle resulting from carbon–iron redox coupling
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March 2011 |
Iron-carbon interactions at high temperatures and pressures
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March 2008 |
Oxygen potential of diamond formation in the lower mantle
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February 2013 |
Experimental investigation on dolomite dissociation into aragonite+magnesite up to 8.5 GPa
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January 2001 |
Stability and equation of state of Fe 3 C to 73 GPa: Implications for carbon in the Earth's core
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May 2001 |
Fate of carbonates within oceanic plates subducted to the lower mantle, and a possible mechanism of diamond formation
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February 2008 |
In situ X-ray observation of the reaction dolomite = aragonite + magnesite at 900–1300 K
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July 2002 |
Diamond formation in metal–carbonate interactions
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January 2005 |
Large gem diamonds from metallic liquid in Earth’s deep mantle
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December 2016 |
Melting and decomposition of MgCO3 at pressures up to 84 GPa
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August 2014 |
Quasi-hydrostatic compression of magnesium oxide to 52 GPa: Implications for the pressure-volume-temperature equation of state
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January 2001 |
Congruent melting of calcium carbonate in a static experiment at 3500 K and 10–22 GPa: Its role in the genesis of ultradeep diamonds
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August 2011 |
The oxygen fugacity at which graphite or diamond forms from carbonate-bearing melts in eclogitic rocks
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February 2015 |
The oxidation state of the mantle and the extraction of carbon from Earth’s interior
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January 2013 |
The stability of magnesite in the transition zone and the lower mantle as function of oxygen fugacity: CARBON/CARBONATE fo2 BUFFER AT HP
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October 2011 |
Experimental determination of siderite stability at high pressure
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August 2013 |
Subducting oceanic crust: The source of deep diamonds
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January 2005 |
Slab melting as a barrier to deep carbon subduction
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January 2016 |
Experimental determination of melting in the systems enstatite-magnesite and magnesite-calcite from 15 to 80 GPa
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August 2014 |
Deep Mantle Cycling of Oceanic Crust: Evidence from Diamonds and Their Mineral Inclusions
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September 2011 |
Magnesite-bearing inclusion assemblage in natural diamond
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June 1996 |
Oceanic Island Basalts and Mantle Plumes: The Geochemical Perspective
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April 2010 |
Primordial metallic melt in the deep mantle: Primordial Metallic Melt
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April 2016 |