Browsing ELibrary by Author "Fei Y."
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Browsing ELibrary by Author "Fei Y."
Now showing items 1-16 of 16
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Li J.; Mao H.K.; Fei Y.; Gregoryanz E.; Eremets M.; Zha C.S. (2002)Polycrystalline Fe3C (cementite) was compressed in a neon pressure medium to 30.5 GPa at 300 K using diamond-anvil cell techniques. Angular dispersive X-ray diffraction of Fe3C was measured using monochromatic synchrotron ...
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Frank M.R.; Fei Y.; Hu J. (2004)The study presented here sought to determine the PVT properties of Ice VII at elevated temperatures and pressures up to 60 GPa using a Mao-Bell type diamond anvil cell with an external Mo-wire resistance heater. The unit ...
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Mibe K.; Kanzaki M.; Kawamoto T.; Matsukage K.N.; Fei Y.; Ono S. (2004)To determine the second critical end point in silicate-H2O systems, a new method for the direct observations of immiscible fluids has been developed using a synchrotron X-ray radiography technique. High-pressure and ...
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Wheeler K.T.; Walker D.; Fei Y.; Minarik W.G.; McDonough W.F. (2006)Measurable uranium (U) is found in metal sulfide liquids in equilibrium with molten silicate at conditions appropriate for a planetary magma ocean: 1-10 GPa, 1750-2100 °C, 0-28 wt% S, and fO2 2 log units below IW. However, ...
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Hirose K.; Fei Y.; Ono S.; Yagi T.; Funakoshi K.I. (2001)Here we report the phase boundary of pyrope garnet (Mg3Al2Si3O12) to Al-bearing silicate perovskite plus corundum, with the highest transition pressure determined by in situ measurements in a multi-anvil apparatus at high ...
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Koch-Muller M.; Fei Y.; Hauri E.; Liu Z. (2001)The incorporation of hydrogen (deuterium) into the coesite structure was investigated at pressures from 3.1 to 7.5 GPa and temperatures of 700, 800, and 1100 °C. Hydrogen could only be incorporated into the coesite structure ...
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Lin J.-F.; Fei Y.; Mao H.-K.; Hemley R.J.; Sturhahn W.; Zhao J. (2004)Magnetic, elastic, thermodynamic, and vibrational properties of the most iron-rich sulfide, Fe3S, known to date have been studied with synchrotron Mossbauer spectroscopy (SMS) and nuclear resonant inelastic X-ray scattering ...
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De S.; Heaney P.J.; Fei Y.; Vicenzi E.P. (2004)The contributions that Rob Hargraves made to paleomagnetism spanned not only great distances (from the Earth to Mars) but a vast expanse in time. His interests in the magnetic character of the Archean Earth led him to ...
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Xie X.; Minitti M.E.; Chen M.; Mao H.O.K.; Wang D.; Shu J.; Fei Y. (2002)A new high-pressure polymorph of merrillite with the structure of trigonal γ-Ca3(PO4)2 was found in the shock-produced veins of the Suizhou meteorite, where it coexists with ringwoodite, majorite, NaAlSi3O8-hollandite, and ...
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Lee S.K.; Cody G.D.; Fei Y.; Mysen B.O. (2004)The structures of sodium silicate and aluminosilicate glasses quenched from melts at high pressure (6–10 GPa) with varying degrees of polymerization (fractions of nonbridging oxygen) were explored using solid-state NMR ...
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Koch-Müller M.; Dera P.; Fei Y.; Reno B.; Sobolev N.; Hauri E.; Wysoczanski R. (2003)The incorporation of hydrogen into the coesite structure was investigated at pressures ranging from 4.0–9.0 GPa and temperatures from 750–1300 °C using Al and B doped SiO2 starting materials. The spectra show four sharp ...
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Sanloup C.; Gillet P.; Guyot F.; Fei Y. (2002)Sulfur and silicon are among the expected alloying light elements in planetary liquid iron cores. Structural properties of Fe-27 wt % S and Fe-17 wt % Si liquid alloys at high pressure and high temperature (0-5 GPa/1400-2300 ...
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Hirose K.; Fei Y. (2002)The phase relations and the element partitioning in a mid-oceanic ridge basalt composition were determined for both above-solidus and subsolidus conditions at 22 to 27.5 GPa by means of a multianvil apparatus. The mineral ...
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Li J.; Fei Y.; Mao H.K.; Hirose K.; Shieh S.R. (2001)Experiments have been conducted to study the Fe-S binary phase diagram near the pure iron end member, at pressures between 7 and 25 GPa and temperatures between 1223 and 1473 K. We observed that more than 1 atomic percent ...
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Konzett J.; Fei Y. (2000)We have investigated the stability and composition of potassium amphibole and its high-pressure breakdown product phase X in synthetic peralkaline and subalkaline KNCMASH (K 2 O–Na 2 O–CaO–MgO–Al 2 O 3 –SiO 2 –H 2 O) and ...
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Konzett Ju.; Fei Y. (2000)We have investigated the stability and composition of potassium amphibole and its high-pressure breakdown product phase X in synthetic peralkaline and subalkaline KNCMASH (K2O–Na2O–CaO–MgO–Al2O3–SiO2–H2O) and natural KLB-1 ...
Now showing items 1-16 of 16
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