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Cited by 983

The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.

U-Th Isotopes in Arc Magmas: Implications for Element Transfer from the Subducted Crust

Hawkesworth, C. J., Turner, S. P., McDermott, F., Peate, D. W., van Calsteren, P.·1997·Science

Abstract

Uranium-thorium isotope results from island arc volcanic rocks were used to investigate the rates of transfer of fluids and sediments from the downgoing slab. Uranium, but not thorium, is readily mobilized in the fluid. A negative array between thorium/cerium and neodymium-143/neodymium-144 indicates that significant amounts of the thorium in arc rocks are derived from subducted sediments, although perhaps only about 30 percent of the thorium in subducted sediments is returned to the crust in this way. The transfer times for fluid through the mantle wedge are about 30,000 to 120,000 years, whereas those for sediment melts may be several million years. The low average uranium/thorium ratios of bulk crust primarily reflect different crustal generation processes in the Archaean.

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Metadata

Authors
Hawkesworth, C. J., Turner, S. P., McDermott, F., Peate, D. W., & van Calsteren, P.
Venue
Science
Published
1997-04-25
Volume
276
Issue
5312
Pages
551-555
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2086820683
Cited by
983
References
2
FWCI
12.43
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: U-Th Isotopes in Arc Magmas: Implications for Element Transfer from the Subducted Crust. https://app.cochat.ai/papers/10.1126/science.276.5312.551
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Hawkesworth, C. J., Turner, S. P., McDermott, F., Peate, D. W., & van Calsteren, P. (1997). U-Th Isotopes in Arc Magmas: Implications for Element Transfer from the Subducted Crust. Science. https://doi.org/10.1126/science.276.5312.551

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