(Q107288535)

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Testing plausible upper-mantle compositions using fine-scale models of the 410-km discontinuity

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Testing plausible upper-mantle compositions using fine-scale models of the 410-km discontinuity (English)

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Yanbin Wang

2

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author name string

James B. Gaherty

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1

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Thomas H. Jordan

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3

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Donald J. Weidner

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4

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publication date

1 June 1999

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published in

Geophysical Research Letters

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volume

26

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issue

11

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page(s)

1641-1644

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cites work

High-pressure phase equilibria in a garnet lherzolite, with special reference to Mg2+Fe2+ partitioning among constituent minerals

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Phase transition Clapeyron slopes and transition zone seismic discontinuity topography

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Elasticity of forsterite to 16 GPa and the composition of the upper mantle

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Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity

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The system Mg2SiO4-Fe2SiO4at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel

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The composition of the Earth

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Upper-mantle seismic discontinuities and the thermal structure of subduction zones

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Mantle discontinuities under southern Africa from precursors to P′ P′df

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(Q107288535)

Testing plausible upper-mantle compositions using fine-scale models of the 410-km discontinuity

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