Experimental constraints on the fate of H and C during planetary core-mantle differentiation. Implications for the Earth

[1]  R. Dasgupta,et al.  Core-mantle fractionation of carbon in Earth and Mars: The effects of sulfur , 2018, Geochimica et Cosmochimica Acta.

[2]  H. Bureau,et al.  Low hydrogen contents in the cores of terrestrial planets , 2018, Science Advances.

[3]  L. Elkins‐Tanton,et al.  The fate of water within Earth and super-Earths and implications for plate tectonics , 2017, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[4]  G. Steinle‐Neumann,et al.  Experimental determination of oxygen diffusion in liquid iron at high pressure , 2017 .

[5]  T. Yagi,et al.  Hydrogenation of iron in the early stage of Earth's evolution , 2017, Nature Communications.

[6]  G. Manthilake,et al.  Effect of H 2 O on metal–silicate partitioning of Ni, Co, V, Cr, Mn and Fe: Implications for the oxidation state of the Earth and Mars , 2016 .

[7]  N. Shimizu,et al.  Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos , 2016 .

[8]  C. Russell,et al.  A partially differentiated interior for (1) Ceres deduced from its gravity field and shape , 2016, Nature.

[9]  H. Keppler,et al.  Molecular hydrogen in mantle minerals , 2016 .

[10]  B. Marty,et al.  Origins of volatile elements (H, C, N, noble gases) on Earth and Mars in light of recent results from the ROSETTA cometary mission , 2016 .

[11]  A. Baron,et al.  Constraints on Earth’s inner core composition inferred from measurements of the sound velocity of hcp-iron in extreme conditions , 2016, Science Advances.

[12]  John H. Jones,et al.  The formation of nuggets of highly siderophile elements in quenched silicate melts at high temperatures: Before or during the silicate quench? , 2016 .

[13]  E. Ohtani Hydrous minerals and the storage of water in the deep mantle , 2015 .

[14]  M. Hirschmann,et al.  Speciation and solubility of reduced C–O–H–N volatiles in mafic melt: Implications for volcanism, atmospheric evolution, and deep volatile cycles in the terrestrial planets , 2015 .

[15]  F. Gaillard,et al.  Effects of temperature, pressure and chemical compositions on the electrical conductivity of carbonated melts and its relationship with viscosity , 2015 .

[16]  M. Mottl,et al.  Evidence for primordial water in Earth’s deep mantle , 2015, Science.

[17]  N. Chabot,et al.  The effect of oxygen as a light element in metallic liquids on partitioning behavior , 2015 .

[18]  Seth Andrew Jacobson,et al.  Accretion and differentiation of the terrestrial planets with implications for the compositions of early-formed Solar System bodies and accretion of water , 2014, 1410.3509.

[19]  H. Terasaki,et al.  Repulsive Nature for Hydrogen Incorporation to Fe3C up to 14 GPa , 2014 .

[20]  Francis M. McCubbin,et al.  Early accretion of water in the inner solar system from a carbonaceous chondrite–like source , 2014, Science.

[21]  F. Gaillard,et al.  A theoretical framework for volcanic degassing chemistry in a comparative planetology perspective and implications for planetary atmospheres , 2014 .

[22]  E. B. Kryukova,et al.  Solution behavior of C-O-H volatiles in FeO-Na2O-Al2O3-SiO2 melts in equilibrium with liquid iron alloy and graphite at 4 GPa and 1550°C , 2014, Geochemistry International.

[23]  N. Shimizu,et al.  Partitioning of carbon between Fe-rich alloy melt and silicate melt in a magma ocean - Implications for the abundance and origin of volatiles in Earth, Mars, and the Moon , 2014 .

[24]  K. Righter,et al.  How Mercury can be the most reduced terrestrial planet and still store iron in its mantle , 2014 .

[25]  H. Terasaki,et al.  High-pressure and high-temperature phase diagram for Fe0.9Ni0.1-H alloy , 2014 .

[26]  F. Robert,et al.  Ion Microprobe Determination of Hydrogen Concentration and Isotopic ratio in Extraterrestrial Metallic Alloys , 2013 .

[27]  V. Prakapenka,et al.  Phase relations in the Fe-FeSi system at high pressures and temperatures , 2013 .

[28]  D. Walker,et al.  Carbon solution and partitioning between metallic and silicate melts in a shallow magma ocean: Implications for the origin and distribution of terrestrial carbon , 2013 .

[29]  B. Marty,et al.  Asteroidal impacts and the origin of terrestrial and lunar volatiles , 2013 .

[30]  B. Marty The origins and concentrations of water, carbon, nitrogen and noble gases on Earth , 2014, 1405.6336.

[31]  M. Hirschmann,et al.  Calibration of infrared spectroscopy by elastic recoil detection analysis of H in synthetic olivine , 2012 .

[32]  Emmanuel Le Trong,et al.  New experimental data and semi-empirical parameterization of H2O–CO2 solubility in mafic melts , 2012 .

[33]  Qing-Zhu Yin,et al.  Carbon and other light element contents in the Earth’s core based on first-principles molecular dynamics , 2012, Proceedings of the National Academy of Sciences.

[34]  M. Hirschmann,et al.  Solubility of molecular hydrogen in silicate melts and consequences for volatile evolution of terrestrial planets , 2012 .

[35]  B. Mysen Silicate-COH melt and fluid structure, their physicochemical properties, and partitioning of nominally refractory oxides between melts and fluids , 2012 .

[36]  Alessandro Morbidelli,et al.  Building Terrestrial Planets , 2012, 1208.4694.

[37]  Y. Ohishi,et al.  Stability of Fe-Ni hydride after the reaction between Fe-Ni alloy and hydrous phase (δ-AlOOH) up to 1.2Mbar: Possibility of H contribution to the core density deficit , 2012 .

[38]  D. Antonangeli,et al.  Metal–silicate partitioning of Ni and Co in a deep magma ocean , 2012 .

[39]  M. Hirschmann,et al.  Solubility of COH volatiles in graphite-saturated martian basalts , 2012 .

[40]  A. Baron,et al.  Sound velocity measurements in dhcp-FeH up to 70 GPa with inelastic X-ray scattering: Implications for the composition of the Earth's core , 2012 .

[41]  L. Dubrovinsky,et al.  X-ray diffraction and Mössbauer spectroscopy study of fcc iron hydride FeH at high pressures and implications for the composition of the Earth's core , 2011 .

[42]  K. Righter,et al.  Terrestrial planet formation , 2011, Proceedings of the National Academy of Sciences.

[43]  H. Terasaki,et al.  Effect of hydrogen on the melting temperature of FeS at high pressure: Implications for the core of Ganymede , 2011 .

[44]  M. Portnyagin,et al.  Solubility of H2O- and CO2-bearing fluids in tholeiitic basalts at pressures up to 500 MPa , 2010 .

[45]  M. Hirschmann,et al.  The deep carbon cycle and melting in Earth's interior , 2010 .

[46]  A. Jambon,et al.  The chemical composition of the Earth: Enstatite chondrite models , 2010 .

[47]  K. Righter,et al.  Partitioning of Mo, P and other siderophile elements (Cu, Ga, Sn, Ni, Co, Cr, Mn, V, and W) between metal and silicate melt as a function of temperature and silicate melt composition , 2010 .

[48]  John H. Jones,et al.  Highly reducing conditions during core formation on Mercury: Implications for internal structure and the origin of a magnetic field , 2010 .

[49]  D. Walker,et al.  High-pressure melting relations in Fe-C-S systems: Implications for formation, evolution, and structure of metallic cores in planetary bodies , 2009 .

[50]  H. Terasaki,et al.  Hydrogen partitioning between iron and ringwoodite: Implications for water transport into the Martian core , 2009 .

[51]  K. Righter,et al.  Melting of the Indarch meteorite (EH4 chondrite) at 1 GPa and variable oxygen fugacity: Implications for early planetary differentiation processes , 2009 .

[52]  S. Clark,et al.  Melting in the Fe–C system to 70 GPa , 2009 .

[53]  H. Bureau,et al.  Determination of hydrogen content in geological samples using elastic recoil detection analysis (ERDA) , 2009 .

[54]  M. Hirschmann,et al.  The H/C ratios of Earth's near-surface and deep reservoirs, and consequences for deep Earth volatile cycles , 2009 .

[55]  Y. Nakajima,et al.  Melting phase relation of FeHx up to 20 GPa: Implication for the temperature of the Earth's core , 2009 .

[56]  G. Cody,et al.  Solution behavior of reduced COH volatiles in silicate melts at high pressure and temperature , 2009 .

[57]  V. Malavergne,et al.  Highly Reducing Conditions During Core Formation on Mercury: Implications for Internal Structure, the Distribution of Heat-Producing Elements and the Origin of a Magnetic Field , 2008 .

[58]  D. Frost,et al.  The Redox State of Earth's Mantle , 2008 .

[59]  L. Stixrude,et al.  Hydrous silicate melt at high pressure , 2008, Nature.

[60]  K. Righter,et al.  Evolution of Indarch (EH4 Chondrite) at 1 GPa and High Temperature , 2008 .

[61]  John H. Jones,et al.  New high-pressure and high-temperature metal/silicate partitioning of U and Pb: Implications for the cores of the Earth and Mars , 2007 .

[62]  A. Jephcoat,et al.  Potassium partitioning into molten iron alloys at high-pressure: Implications for Earth's core , 2006 .

[63]  B. Wood,et al.  Accretion of the Earth and segregation of its core , 2006, Nature.

[64]  T. Kikegawa,et al.  Iron-water reaction at high pressure and temperature, and hydrogen transport into the core , 2005 .

[65]  H. Fukui,et al.  Decomposition of brucite up to 20 GPa: evidence for high MgO-solubility in the liquid phase , 2005 .

[66]  S. Saxena,et al.  Formation of iron hydride and high-magnetite at high pressure and temperature , 2004 .

[67]  Tomoaki Kubo,et al.  Phase relations of a carbonaceous chondrite at lower mantle conditions , 2004 .

[68]  L. Daudin,et al.  Development of “position–charge–time” tagged spectrometry for ion beam microanalysis , 2003 .

[69]  F. Guyot,et al.  The behaviour of sulphur in metal–silicate core segregation experiments under reducing conditions , 2003 .

[70]  S. Eggins,et al.  The effect of melt composition on trace element partitioning: an experimental investigation of the activity coefficients of FeO, NiO, CoO, MoO2 and MoO3 in silicate melts , 2002 .

[71]  D. Frost,et al.  Peridotite melting and mineral–melt partitioning of major and minor elements at 22–24.5 GPa , 2002 .

[72]  E. Berthoumieux,et al.  The Pierre Süe Laboratory nuclear microprobe as a multi-disciplinary analysis tool , 2001 .

[73]  Zhongting Ma Thermodynamic description for concentrated metallic solutions using interaction parameters , 2001 .

[74]  M. Mayer SIMNRA, a simulation program for the analysis of NRA, RBS and ERDA , 1999 .

[75]  T. Okuchi,et al.  Hydrogen partitioning into molten iron at high pressure: implications for Earth's core , 1997, Science.

[76]  S. Chakraborty,et al.  The activities of NiO, CoO and FeO in silicate melts , 1997 .

[77]  C. Agee,et al.  Pressure‐temperature phase diagram for the Allende meteorite , 1995 .

[78]  T. Yagi,et al.  Iron hydride formed by the reaction of iron, silicate, and water: Implications for the light element of the Earth's core , 1995 .

[79]  J. Poirier Light elements in the Earth's outer core: A critical review , 1994 .

[80]  T. Nagasaka,et al.  Phase Equilibria of Liquid Fe-S-C Ternary System , 1991 .

[81]  H. Mao,et al.  High-Pressure Chemistry of Hydrogen in Metals: In Situ Study of Iron Hydride , 1991, Science.

[82]  C. Agee,et al.  Partitioning “equilibrium”, temperature gradients, and constraints on Earth differentiation , 1989 .

[83]  D. Vrnco Relationships between properties and structure of aluminosilicate melts , 1985 .

[84]  Y. Fukai The iron–water reaction and the evolution of the Earth , 1984, Nature.

[85]  C. Hazard,et al.  The Earth's core , 1977, Nature.

[86]  L. Pepkowitz,et al.  DETERMINATION OF HYDROGEN , 1949 .