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Nd isotopic variations and petrogenetic models

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

Abstract

The decay of 147 Sm to 143 Nd allows 143 Nd/144 Nd to be used to trace Sm/Nd fractionation in long time‐scale geologic processes. 143 Nd/144 Nd has been measured in terrestrial rock samples of different ages to establish the characteristics of Nd isotopic evolution in the crust and mantle. The evolution of 143 Nd/144 Nd in the mantle indicates Sm/Nd essentially equal to that of chondrites, and implies a chondritic REE distribution for the earth. Variations in 143 Nd/144 Nd do exist in the mantle, however, indicating Sm/Nd heterogeneity and the existence of distinct mantle reservoirs with characteristic 143 Nd/144 Nd. 143 Nd/144 Nd in average crustal rocks today is much lower than found in recent mantle samples and reflects their age and low Sm/Nd. Oceanic tholeiites and alkali basalt are derived from sources with Sm/Nd which has been 5‐10% greater than chondritic over the age of the earth. Alkali basalt can not be derived from mantle reservoirs which have been light REE‐enriched for long times.

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Metadata

Authors
DePaolo, D. J., & Wasserburg, G. J.
Venue
Geophysical Research Letters
Published
1976-05
Volume
3
Issue
5
Pages
249-252
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2073426602
Cited by
1,229
References
0
FWCI
21.70
Type
journal article
Language
en
Open access
bronze

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DePaolo, D. J., & Wasserburg, G. J. (1976). Nd isotopic variations and petrogenetic models. Geophysical Research Letters. https://doi.org/10.1029/gl003i005p00249

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