The DOI matches its Crossref record; 5 of the 5 references it cites were found in a registry or an index.
Correlated microanalysis of zircon: Trace element, δ18O, and U–Th–Pb isotopic constraints on the igneous origin of complex >3900Ma detrital grains
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Cites
Wilde, S. A., Valley, J. W., Peck, W. H., & Graham, C. M. (2001) · Nature · doi:10.1038/35051550 · Cited by 1,744 · cited 12×
“When the above ‘unreliable’ analyses ( 33% of all analyses) are excluded, the range in values from concordant domains is 4.6& to 7.3&, with one outlier at 10.3& (Peck et al., 2001; Wilde et al., 2001; Cavosie et al., 2005).”
BackgroundMethodInfluentialSelf-citation4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon
Valley, J. W., Lackey, J. S., Cavosie, A. J., Clechenko, C. C., Spicuzza, M. J., Basei, M. A. S., Bindeman, I. N., Ferreira, V. P., Sial, A. N., King, E. M., et al. (2005) · Contributions to Mineralogy and Petrology · doi:10.1007/s00410-005-0025-8 · Cited by 1,222
Self-citationZircon Thermometer Reveals Minimum Melting Conditions on Earliest Earth
Watson, E. B., & Harrison, T. M. (2005) · Science · doi:10.1126/science.1110873 · Cited by 955
Oxygen-isotope evidence from ancient zircons for liquid water at the Earth's surface 4,300 Myr ago
Mojzsis, S. J., Harrison, T. M., & Pidgeon, R. T. (2001) · Nature · doi:10.1038/35051557 · Cited by 863
Priscoan (4.00–4.03 Ga) orthogneisses from northwestern Canada
Bowring, S. A., & Williams, I. S. (1999) · Contributions to Mineralogy and Petrology · doi:10.1007/s004100050465 · Cited by 568 · cited 2×
“While no intact rocks older than 4030 Ma are known (Bowring and Williams, 1999), the chemical compositions of these detrital grains have been used to make inferences about the composition, petrogenesis, and geologic history of the original host rocks to the zircons, which provide insights into…”
Background
Cited by
Ce and Eu anomalies in zircon as proxies for the oxidation state of magmas
Trail, D., Bruce Watson, E., & Tailby, N. D. (2012) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2012.08.032 · Cited by 787
Hazen, R. M., Papineau, D., Bleeker, W., Downs, R. T., Ferry, J. M., McCoy, T. J., Sverjensky, D. A., & Yang, H. (2008) · American Mineralogist · doi:10.2138/am.2008.2955 · Cited by 701
The oxidation state of Hadean magmas and implications for early Earth’s atmosphere
Trail, D., Watson, E. B., & Tailby, N. D. (2011) · Nature · doi:10.1038/nature10655 · Cited by 613
Diffusion in Accessory Minerals: Zircon, Titanite, Apatite, Monazite and Xenotime
Cherniak, D. J. (2010) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2010.72.18 · Cited by 328
The Hadean-Archaean Environment
Sleep, N. H. (2010) · Cold Spring Harbor Perspectives in Biology · doi:10.1101/cshperspect.a002527 · Cited by 228
Metadata
- Authors
- Cavosie, A. J., Valley, J. W., & Wilde, S. A.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2006-11
- Volume
- 70
- Issue
- 22
- Pages
- 5601-5616
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2171880560
- Cited by
- 193
- References
- 5
- FWCI
- 7.92
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: Correlated microanalysis of zircon: Trace element, δ18O, and U–Th–Pb isotopic constraints on the igneous origin of complex >3900Ma detrital grains. https://app.cochat.ai/papers/10.1016/j.gca.2006.08.011
- The paper
- Cavosie, A. J., Valley, J. W., & Wilde, S. A. (2006). Correlated microanalysis of zircon: Trace element, δ18O, and U–Th–Pb isotopic constraints on the igneous origin of complex >3900Ma detrital grains. Geochimica et Cosmochimica Acta. https://doi.org/10.1016/j.gca.2006.08.011
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
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.
