(Q59024046)

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Neodymium isotope evidence for ultra-depleted mantle in the early Proterozoic

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Neodymium isotope evidence for ultra-depleted mantle in the early Proterozoic (English)

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W. J. Sivell

1

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M. T. McCulloch

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2

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language of work or name

English

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publication date

December 1991

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published in

Nature

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volume

354

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issue

6352

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page(s)

384-387

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exact match

https://scigraph.springernature.com/pub.10.1038/354384a0

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Neodymium isotopes in the Colorado Front Range and crust–mantle evolution in the Proterozoic

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Sm–Nd age of Kambalda and Kanowna greenstones and heterogeneity in the Archaean mantle

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Banded amphibolites of the harts range meta-igneous complex, central Australia: an early proterozoic basalt-tonalite suite

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The Entire anorthositic gneiss, eastern Arunta Inlier, Central Australia: Geochemistry and petrogenesis

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1,700-Myr greenstone volcanic successions in southwestern North America and isotopic evolution of Proterozoic mantle

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Geochemical and geodynamical constraints on subduction zone magmatism

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Nd isotopic variations and petrogenetic models

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Evidence for extreme mantle fractionation in early Archaean ultramafic rocks from northern Labrador

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Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes

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Amphibolites from the Entia Gneiss Complex, Eastern Arunta inlier: Geochemical evidence for a proterozoic transition from extensional to compressional tectonics

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The petrology and geochemistry of granitic gneisses from the East Arunta inlier, central Australia: implications for Proterozoic crustal development

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The Pleistocene-Recent Tonga-Kermadec Arc Lavas: Interpretation of New Isotopic and Rare Earth Data in Terms of a Depleted Mantle Source Model

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Nd isotopic characteristics of S- and I-type granites

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10.1038/354384A0

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1034555689

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(Q59024046)

Neodymium isotope evidence for ultra-depleted mantle in the early Proterozoic

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