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Inferences about magma sources and mantle structure from variations of 143Nd/144Nd

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DePaolo, D. J., Wasserburg, G. J.·1976·Geophysical Research Letters

Abstract

Continental flood basalts and mid‐ocean ridge (MOR) tholeiitic basalts have distinctly different 143 Nd/144 Nd which may permit a priori distinction between "continental" and "oceanic" igneous rocks. Initial 143 Nd/144 Nd of continental igneous rocks through time fall on a Sm/Nd evolution curve with chondritic REE abundance ratio. These observations indicate that many continental igneous rocks are derived from a reservoir with chondritic REE pattern which may represent primary material remaining since the formation of the earth. Oceanic igneous rocks are derived from a different ancient reservoir which has Sm/Nd higher than chondritic. Initial 143 Nd/144 Nd and 87 Sr/86 Sr in young basalts from both oceans and continents show a strong correlation suggesting that Sm‐Nd and Rb‐Sr fractionation events in the mantle may be correlative and caused by the same process. From this correlation Rb/Sr for the earth is inferred to be 0.029.

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Metadata

Authors
DePaolo, D. J., & Wasserburg, G. J.
Venue
Geophysical Research Letters
Published
1976-12
Volume
3
Issue
12
Pages
743-746
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2156321503
Cited by
652
References
2
FWCI
19.92
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Inferences about magma sources and mantle structure from variations of 143Nd/144Nd. https://app.cochat.ai/papers/10.1029/gl003i012p00743
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DePaolo, D. J., & Wasserburg, G. J. (1976). Inferences about magma sources and mantle structure from variations of 143Nd/144Nd. Geophysical Research Letters. https://doi.org/10.1029/gl003i012p00743

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