(Q107275318)

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The Effect of Temperature on the Partitioning of Nickel, Cobalt, Manganese, Chromium, and Vanadium at 9 GPa and Constraints on Formation of the Earth’s Core

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scholarly article

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The Effect of Temperature on the Partitioning of Nickel, Cobalt, Manganese, Chromium, and Vanadium at 9 GPa and Constraints on Formation of the Earth’s Core (English)

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author name string

Christine K. Geßmann

1

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David C. Rubie

2

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publication date

March 1998

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Geochimica et Cosmochimica Acta

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62

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5

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867-882

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Pressure-temperature phase diagram for the Allende meteorite

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High-pressure and high-temperature experiments on core-mantle segregation in the accreting Earth

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The mineralogy and chemistry of the lower mantle: an implication of the ultrahigh-pressure phase relations in the system MgOFeOSiO2

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Reactions between molten iron and silicate melts at high pressure: Implications for the chemical evolution of Earth's core

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Geochemical constraints on core formation in the Earth

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Experimental determination of element partitioning between silicate perovskites, garnets and liquids: constraints on early differentiation of the mantle

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Pressure-induced coordination changes of transition-metal ions in silicate melts

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Partitioning of MgO, FeO, NiO, MnO and Cr2O3 between magnesian silicate perovskite and magnesiowüstite: implications for the origin of inclusions in diamond and the composition of the lower mantle

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Geochemistry of mantle–core differentiation at high pressure

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Partitioning of nickel, cobalt and manganese between silicate perovskite and periclase: a test of crystal field theory at high pressure

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The composition of the Earth

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Element partitioning between Mg-perovskite, magnesiowüstite, and silicate melt at conditions of the Earth's mantle

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Early differentiation of the Earth and the problem of mantle siderophile elements: a new approach

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Oxide-metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's core

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Composition of the core, I. Solubility of oxygen in molten iron at high temperatures

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Element partitioning between metallic liquid, silicate liquid, and lower-mantle minerals: implications for core formation of the Earth

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Light elements in the Earth's outer core: A critical review

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Activities in Solid and Liquid Fe  Ni and Fe  Co Alloys Determined by Knudsen Cell Mass Spectrometry

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High-pressure geochemistry of Cr, V and Mn and implications for the origin of the Moon

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Activity-composition relations of the magnesiowüstite solid solution series in equilibrium with metallic iron in the temperature range 1050–1400 K

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The influence of pressure and temperature on the metal-silicate partition coefficients of nickel and cobalt in a model C1 chondrite and implications for metal segregation in a deep magma ocean

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Element partitioning between silicate minerals and coexisting melts at pressures of 1–27 GPa, and implications for mantle evolution

1 reference

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Partitioning of Ni between magnesiowüstite and metal at high pressure: implications for core-mantle equilibrium

1 reference

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Superheating effects on metal-silicate partitioning of siderophile elements

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Identifiers

10.1016/S0016-7037(98)00023-4

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1998GeCoA..62..867G

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