(Q63947435)

English

High-pressure and high-temperature reactions between silicates and liquid iron alloys, in the diamond anvil cell, studied by analytical electron microscopy

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scholarly article

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High-pressure and high-temperature reactions between silicates and liquid iron alloys, in the diamond anvil cell, studied by analytical electron microscopy (English)

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author name string

Francoise Goarant

1

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Francois Guyot

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Jean Peyronneau

3

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Jean-Paul Poirier

4

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publication date

1992

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Journal of Geophysical Research

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97

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B4

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4477

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X-ray microanalysis of high-pressure/high-temperature phases synthesized from natural olivine in a diamond-anvil cell

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Shock-produced olivine glass: first observation

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Earth's Core-Mantle Boundary: Results of Experiments at High Pressures and Temperatures

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Structure of the core-mantle transition zone

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Eutectoid phase transformation of olivine and spinel into perovskite and rock salt structures

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

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Models of the Earth's Core

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The Melting Curve of Iron to 250 Gigapascals: A Constraint on the Temperature at Earth's Center

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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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Electron microscopy of high-pressure phases synthesized from natural olivine in diamond anvil cell

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The Bakerian Lecture, 1983 - The Earth’s core: its composition, formation and bearing upon the origin of the Earth

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Solubilities of mantle oxides in molten iron at high pressures and temperatures: implications for the composition and formation of Earth's core

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Identifiers

10.1029/92JB00018

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1992JGR....97.4477G

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