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U-Th Isotopes in Arc Magmas: Implications for Element Transfer from the Subducted Crust
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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Citations
Cites
Nature and composition of the continental crust: A lower crustal perspective
Rudnick, R. L., & Fountain, D. M. (1995) · Reviews of Geophysics · doi:10.1029/95rg01302 · Cited by 3,323
Tracing trace elements from sediment input to volcanic output at subduction zones
Plank, T., & Langmuir, C. H. (1993) · Nature · doi:10.1038/362739a0 · Cited by 744
Cited by
Stern, R. J. (2002) · Reviews of Geophysics · doi:10.1029/2001rg000108 · Cited by 1,517
Dilek, Y., & Furnes, H. (2011) · Geological Society of America Bulletin · doi:10.1130/b30446.1 · Cited by 1,167
Special Paper: Adakite-Like Rocks: Their Diverse Origins and Questionable Role in Metallogenesis
Richards, J. P., & Kerrich, R. (2007) · Economic Geology · doi:10.2113/gsecongeo.102.4.537 · Cited by 964
Dilek, Y., & Furnes, H. (2014) · Elements · doi:10.2113/gselements.10.2.93 · Cited by 689
Subduction styles in the Precambrian: Insight from numerical experiments
Sizova, E., Gerya, T., Brown, M., & Perchuk, L. L. (2010) · Lithos · doi:10.1016/j.lithos.2009.05.028 · Cited by 441
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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- 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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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.