Centrifuge assisted percolation of Fe–S melts in partially molten peridotite: Time constraints for planetary core formation
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[1] H. Terasaki,et al. In situ measurement of interfacial tension of Fe-S and Fe-P liquids under high pressure using X-ray radiography and tomography techniques , 2009 .
[2] A. Halliday. A young Moon-forming giant impact at 70–110 million years accompanied by late-stage mixing, core formation and degassing of the Earth , 2008, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[3] H. Terasaki,et al. Percolative core formation in planetesimals , 2008 .
[4] R. Hough,et al. Three-dimensional morphology of magmatic sulfides sheds light on ore formation and sulfide melt migration , 2008 .
[5] G. Manhès,et al. The major differentiation of the Earth at ∼ 4.45 Ga , 2008 .
[6] F. Nimmo,et al. How rapidly did Mars accrete? Uncertainties in the Hf-W timing of core formation , 2007 .
[7] P. Bons,et al. Liquid-distribution and attainment of textural equilibrium in a partially-molten crystalline system with a high-dihedral-angle liquid phase , 2007 .
[8] J. Kinney,et al. Fe‐Ni‐S melt permeability in olivine: Implications for planetary core formation , 2007 .
[9] C. Liebske,et al. Mars: A New Core-Crystallization Regime , 2007, Science.
[10] H. Terasaki,et al. Interconnectivity of Fe O S liquid in polycrystalline silicate perovskite at lower mantle conditions , 2007 .
[11] D. Günther,et al. Element Partitioning: The Role of Melt Structure and Composition , 2006, Science.
[12] B. Wood,et al. Accretion of the Earth and segregation of its core , 2006, Nature.
[13] F. Nimmo,et al. Isotopic outcomes of N-body accretion simulations: Constraints on equilibration processes during large impacts from Hf/W observations , 2006 .
[14] R. Ando,et al. Viscosity of peridotite liquid up to 13 GPa: Implications for magma ocean viscosities , 2005 .
[15] Klaus Mezger,et al. Hf-W Chronometry of Lunar Metals and the Age and Early Differentiation of the Moon , 2005, Science.
[16] N. Petford,et al. Fe-liquid segregation in deforming planetesimals: Coupling Core-Forming compositions with transport phenomena , 2005 .
[17] B. Wood,et al. Cooling of the Earth and core formation after the giant impact , 2005, Nature.
[18] B. Wood,et al. Core formation and the oxidation state of the Earth , 2005 .
[19] R. Carlson,et al. 142Nd Evidence for Early (>4.53 Ga) Global Differentiation of the Silicate Earth , 2005, Science.
[20] E. Watson,et al. Growth kinetics of FeS melt in partially molten peridotite: An analog for core-forming processes , 2005 .
[21] A. Jambon,et al. Widespread magma oceans on asteroidal bodies in the early Solar System , 2005, Nature.
[22] J. Mungall,et al. Interfacial tension between magmatic sulfide and silicate liquids: Constraints on kinetics of sulfide liquation and sulfide migration through silicate rocks , 2005 .
[23] D. Kohlstedt,et al. The Effect of Large Melt Fraction on the Deformation Behavior of Peridotite: Implications for the Viscosity of Io's Mantle and the Rheologically Critical Melt Fraction , 2004 .
[24] M. Walter,et al. Early Earth Differentiation , 2004, Science.
[25] C. McCammon,et al. A redox profile of the Slave mantle and oxygen fugacity control in the cratonic mantle , 2004 .
[26] J. Chambers. Planetary accretion in the inner Solar System , 2004 .
[27] T. Kleine,et al. 182Hf-182W isotope systematics of chondrites, eucrites, and martian meteorites: Chronology of core formation and early mantle differentiation in Vesta and Mars , 2004 .
[28] T. Yoshino,et al. Connectivity of molten Fe alloy in peridotite based on in situ electrical conductivity measurements: implications for core formation in terrestrial planets , 2004 .
[29] D. Kohlstedt,et al. Rheological Properties of Partially Molten Lherzolite , 2004 .
[30] M. Walter. 2.08 – Melt Extraction and Compositional Variability in Mantle Lithosphere , 2003 .
[31] D. Kohlstedt,et al. Metal‐silicate segregation in deforming dunitic rocks , 2003 .
[32] T. Yoshino,et al. Core formation in planetesimals triggered by permeable flow , 2003, Nature.
[33] Kevin Righter,et al. Mechanisms of metal-silicate equilibration in the terrestrial magma ocean , 2003 .
[34] S. Sutton,et al. Viscosity and density of Fe–S liquids at high pressures , 2002 .
[35] T. Spohn,et al. Numerical Modeling of 26Al-Induced Radioactive Melting of Asteroids Considering Accretion , 2002 .
[36] K. Mezger,et al. Rapid accretion and early core formation on asteroids and the terrestrial planets from Hf–W chronometry , 2002, Nature.
[37] G. Schubert,et al. A two-phase model for compaction and damage: 2. Applications to compaction, deformation, and the role of interfacial surface tension , 2001 .
[38] Xin-She Yang. Density-driven compactional flow in porous media , 2001, 1003.5300.
[39] H. Terasaki,et al. Radiographic study on the viscosity of the Fe-FeS melts at the pressure of 5 to 7 GPa , 2001 .
[40] J. Russell,et al. Chemical stratification of cratonic lithosphere: constraints from the Northern Slave craton, Canada , 2000 .
[41] M. Schmitz,et al. Textural equilibria of iron sulfide liquids in partly molten silicate aggregates and their relevance to core formation scenarios , 2000 .
[42] D. Bruhn,et al. An interconnected network of core-forming melts produced by shear deformation , 2000, Nature.
[43] G. Gaetani,et al. Wetting of mantle olivine by sulfide melt: implications for Re/Os ratios in mantle peridotite and late-stage core formation , 1999 .
[44] M. Ghiorso,et al. Calculation of Peridotite Partial Melting from Thermodynamic Models of Minerals and Melts. III. Controls on Isobaric Melt Production and the Effect of Water on Melt Production , 1999 .
[45] H. McSween,et al. A Thermal Model for the Differentiation of Asteroid 4 Vesta, Based on Radiogenic Heating☆ , 1998 .
[46] UK.,et al. First-principles simulations of liquid Fe-S under Earth's core conditions , 1998, cond-mat/9804035.
[47] U. Faul. Permeability of partially molten upper mantle rocks from experiments and percolation theory , 1997 .
[48] Y. Fei,et al. Mineralogy of the Martian interior up to core‐mantle boundary pressures , 1997 .
[49] D. Dingwell,et al. Modelling of melt segregation processes by high-temperature centrifuging of partially molten granites—II. Rayleigh-Taylor instability and sedimentation , 1996 .
[50] D. Dingwell,et al. Modelling of melt segregation processes by high‐temperature centrifuging of partially molten granites—I. Melt extraction by compaction and deformation , 1996 .
[51] C. Ballhaus,et al. Mobility of core melts during Earth's accretion , 1996 .
[52] Frederick J. Ryerson,et al. Textural Entrapment of Core-Forming Melts , 1996, Science.
[53] I. Sumita,et al. A model for sedimentary compaction of a viscous medium and its application to inner-core growth , 1996 .
[54] Claude J. Allègre,et al. The age of the Earth , 1995 .
[55] G. J. Taylor. Core formation in asteroids , 1992 .
[56] H. Melosh,et al. Core formation by giant impacts , 1991 .
[57] D. McKenzie. Some remarks on the movement of small melt fractions in the mantle , 1989 .
[58] John H. Jones,et al. Geochemical constraints on core formation in the Earth , 1986, Nature.
[59] D. McKenzie,et al. The Generation and Compaction of Partially Molten Rock , 1984 .
[60] P. Roeder,et al. Plagioclase buoyancy in basaltic liquids as determined with a centrifuge furnace , 1978 .
[61] T. Usselman. Experimental approach to the state of the core; Part I, The liquidus relations of the Fe-rich portion of the Fe-Ni-S system from 30 to 100 kb , 1975 .
[62] R. Canup,et al. Origin of the earth and moon , 2000 .
[63] R. Canup,et al. Accretion of the Terrestrial Planets and the Earth-Moon System , 1998 .
[64] J. Li,et al. Geochemistry of mantle–core differentiation at high pressure , 1996, Nature.
[65] D. Stevenson. Fluid Dynamics of Core Formation , 1990 .
[66] H. Melosh. Giant impacts and the thermal state of the early earth , 1990 .
[67] John H. Jones,et al. Origin of the earth , 1990 .
[68] Alfred Edward Ringwood,et al. Origin of the Earth and Moon , 1979 .
[69] G. Wetherill. Radiometric Chronology of the Early Solar System , 1975 .
[70] P. M. Bell,et al. Melting relations in the Fe-rich portion of the system FezFeS at 30 kb pressure , 1969 .