(Q59056462)

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Seismic evidence for a 920-km discontinuity in the mantle

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Seismic evidence for a 920-km discontinuity in the mantle (English)

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author name string

Hitoshi Kawakatsu

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1

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Fenglin Niu

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2

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English

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publication date

September 1994

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published in

Nature

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volume

371

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issue

6495

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page(s)

301-305

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exact match

https://scigraph.springernature.com/pub.10.1038/371301a0

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Preliminary reference Earth model

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Traveltimes for global earthquake location and phase identification

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Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications

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Global mapping of topography on the 660-km discontinuity

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

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Sharpness of upper-mantle discontinuities determined from high-frequency reflections

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A detailed map of the 660-kilometer discontinuity beneath the izu-bonin subduction zone

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Seismic imaging of upper-mantle structure with new evidence for a 520-km discontinuity

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Nature of the 650–km seismic discontinuity: implications for mantle dynamics and differentiation

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Absence of an aluminous phase in the upper part of the Earth's lower mantle

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Electron microscopy of (Mg, Fe)SiO3Perovskite: Evidence for structural phase transitions and implications for the lower mantle

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Stability of orthorhombic MgSiO3 perovskite in the Earth's lower mantle

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Deep Slabs, Geochemical Heterogeneity, and the Large-Scale Structure of Mantle Convection: Investigation of an Enduring Paradox

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DOI

10.1038/371301A0

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1034999474

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(Q59056462)

Seismic evidence for a 920-km discontinuity in the mantle

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