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Mercury's molten core


, : Mercury's molten core. Geoscientist 17(7): 6-7


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Accession: 023021540

DOI: 10.1126/science.316.5825.657c

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Related references

Riner, M.A.; Bina, C.R.; Robinson, M.S.; Desch, S.J., 2008: Internal structure of Mercury; implications of a molten core. Journal of Geophysical Research 113.E8

Margot, J.L.; Peale, S.J.; Jurgens, R.F.; Slade, M.A.; Holin, I.V., 2007: Large longitude libration of Mercury reveals a molten core. Observations of radar speckle patterns tied to the rotation of Mercury establish that the planet occupies a Cassini state with obliquity of 2.11 +/- 0.1 arc minutes. The measurements show that the planet exhibits librations in longitude that are f...

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Barkin, Y.V., 2009: The mechanism of translational displacements of the core of the Earth at inversion molten and solidification of substance at core-mantle boundary in opposite hemispheres. Geophysical Research Abstracts 11

Vocadlo Lidunka, 2007: Ab initio calculations of the elasticity of iron and iron alloys at inner core conditions; evidence for a partially molten inner core?. Ab initio finite temperature molecular dynamics simulations have been used to calculate the elasticity of hcp-Fe, bcc-Fe, FeS and FeSi at core conditions. The calculated compressional wave velocities are in excellent agreement with the most recent...

Khan A.; Mosegaard K.; Williams J.G.; Lognonne P., 2005: The core of the Moon; molten or solid?. Abstracts of Papers Submitted to the Lunar and Planetary Science Conference 36: (unpaginated

M.J.S.J.hnston; R.G.J.S.rens, 1973: Electrical conductivity of molten Fe-Ni-S-C core mix. The electrical conductivity of liquid (Fe90Ni10)3S2 saturated with 2.6 weight percent carbon averages 2.7·105 mho/m at 1000°C and zero pressure. This may imply a slightly lower electrical conductivity for the earth's core than that obtained...

Williams J.G.; Boggs D.H.; Ratcliff J.T.; Dickey J.O., 1999: The Moon's molten core and tidal Q. Analysis of Lunar Laser Ranges reveals signatures due to a liquid core as well as to solid-body tides. The estimated upper limit for core radius is 352 km for pure iron. Tidal dissipation is strong; Q at one month is 37.

Loper David E.; Fearn David R., 1983: A seismic model of a partially molten inner core. An improved model of bulk anelasticity including the effect of thermal and material diffusion, quantitatively capable of explaining the observed anelasticity. Also, studies of the reflection of seismic waves from the inner-core boundary are used t...

Lockhart, W.L.; Macdonald, R.W.; Outridge, P.M.; Wilkinson, P.; Delaronde, J.B.; Rudd, J.W.M., 2000: Tests of the fidelity of lake sediment core records of mercury deposition to known histories of mercury contamination. There has been recent controversy over the discrimination between natural and anthropogenic loadings of mercury to lakes. Sediment core profiles have been interpreted as evidence that inputs to lakes have increased. Some investigators have argued,...