(Q59038667)

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Experimental evidence for the origin of lead enrichment in convergent-margin magmas

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Experimental evidence for the origin of lead enrichment in convergent-margin magmas (English)

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1 reference

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James M. Brenan

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Henry F. Shaw

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2

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Frederick J. Ryerson

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3

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language of work or name

English

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publication date

November 1995

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published in

Nature

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volume

378

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issue

6552

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page(s)

54-56

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exact match

https://scigraph.springernature.com/pub.10.1038/378054a0

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Nb and Pb in oceanic basalts: new constraints on mantle evolution

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7 January 2021

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Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust

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Cerium/lead and lead isotope ratios in arc magmas and the enrichment of lead in the continents

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Experimental evidence for very low solubility of rare-earth elements in C02-rich fluids at mantle conditions

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Prediction of crystal–melt partition coefficients from elastic moduli

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Effect of steeper Archean geothermal gradient on geochemistry of subduction-zone magmas

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Partial melting of amphibolite/eclogite and the origin of Archean trondhjemites and tonalites

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7 January 2021

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Partial melting of two amphibolites: contrasting experimental results under fluid-absent conditions

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7 January 2021

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Dehydration-melting of amphibolite at 10 kbar: the effects of temperature and time

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7 January 2021

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Th, Pb, and Sr isotope variations in young island arc volcanics and oceanic sediments

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7 January 2021

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DOI

10.1038/378054A0

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1003296298

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(Q59038667)

Experimental evidence for the origin of lead enrichment in convergent-margin magmas

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