(Q59099321)

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Constraints on mantle melting at mid-ocean ridges from global 238U–230Th disequilibrium data

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Constraints on mantle melting at mid-ocean ridges from global 238U–230Th disequilibrium data (English)

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T. Elliott

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Charles H. Langmuir

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4

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C. H. Langmuir

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B. Bourdon

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1

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A. Zindler

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2

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language of work or name

English

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publication date

November 1996

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published in

Nature

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volume

384

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issue

6606

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page(s)

231-235

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cites work

Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness

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7 January 2021

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Uranium–thorium disequilibria and partitioning on melting of garnet peridotite

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7 January 2021

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Thorium-Uranium Fractionation by Garnet: Evidence for a Deep Source and Rapid Rise of Oceanic Basalts

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226Ra excesses in mid-ocean-ridge basalts and mantle melting

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7 January 2021

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Geochemical and Isotopic Evidence for Crustal Assimilation Beneath Krafla, Iceland

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A possible role for garnet pyroxenite in the origin of the "garnet signature" in MORB

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Hydrous partial melting of lherzolite at 1 GPa: The effect of H2O on the genesis of basaltic magmas

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7 January 2021

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Sr and Nd isotope geochemistry of oceanic basalts and mantle evolution

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7 January 2021

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Implications of a two-component marble-cake mantle

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7 January 2021

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Iceland Mantle Plume: Geochemical Study of Reykjanes Ridge

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7 January 2021

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10.1038/384231A0

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1003471553

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(Q59099321)

Constraints on mantle melting at mid-ocean ridges from global 238U–230Th disequilibrium data

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