Cited by 706Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisGeological and Geophysical Studies

HfNdSr isotopes and incompatible element abundances in island arcs: implications for magma origins and crust-mantle evolution

White, William M., Patchett, Jonathan·1984·Earth and Planetary Science Letters

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Crossref · 10.1016/0012-821x(84)90112-2

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  • Major fractionation of rare earth elements is accomplished during igneous differentiation of rocks from the mantle, resulting in lower parent-to-daughter ratios of crustal products for both the 147Sm/143Nd and 176Lu/177Hf systematics.

    “The major fractionation of REE is accomplished during igneous differentiation of rocks from the mantle, resulting in lower parent-to-daughter ratios of the crustal products for both the 147Sm/143Nd (McCulloch and Wasserburg, 1978) and the 176Lu/177Hf (White and Patchett, 1982) systematics.”

    From Evolution of Sedimentary Rocks (2014) · cites this paper as White and Patchett, 1982

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Authors
White, W. M., & Patchett, J.
Affiliations
Max Planck Institute for Chemistry (DE)
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
1984-02
Volume
67
Issue
2
Pages
167-185
ISSN
0012-821X (ISSN-L)
OpenAlex
W1989475913
Cited by
706
References
0
Citations by year
2026: 5 · 2025: 8 · 2024: 6 · 2023: 6 · 2022: 15 · 2021: 8 · 2020: 12 · 2019: 14 · 2018: 13 · 2017: 16 · 2016: 16 · 2015: 22 · 2014: 6 · 2013: 11 · 2012: 13
FWCI
25.41
Type
journal article
Language
en
Open access
closed
Locations
Earth and Planetary Science Letters (publishedVersion)
Funders
U.S. Geological Survey
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
Keywords
island arc magmas, magma genesis, continental crust contamination, incompatible trace elements, rare earth elements, negative Ce anomaly, ocean island basalts, subduction zone, sediment recycling, Izu-Bonin arc, Aleutian arc

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