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- W2085205923 endingPage "1723" @default.
- W2085205923 startingPage "1720" @default.
- W2085205923 abstract "The density of $ensuremath{varepsilon}$-iron has been calculated at pressures and temperatures up to 300 GPa and 1300 K, respectively. We observe $ensuremath{varepsilon}$ to $ensuremath{beta}$ phase transition at pressures between 135 and 300 GPa and temperature above 1350 K; the pattern can be interpreted in terms of double hexagonal close-packed structure. The density calculated at high pressure and temperature (330--360 GPa and 5000--7000 K) closely matches with preliminary reference Earth model density, thereby imposing constraint on the composition of the Earth's inner core." @default.
- W2085205923 created "2016-06-24" @default.
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- W2085205923 date "2000-02-21" @default.
- W2085205923 modified "2023-09-27" @default.
- W2085205923 title "<i>In Situ</i>X-Ray Study of Thermal Expansion and Phase Transition of Iron at Multimegabar Pressure" @default.
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- W2085205923 doi "https://doi.org/10.1103/physrevlett.84.1720" @default.
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