The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.
THE R e-O s ISOTOPE SYSTEM IN COSMOCHEMISTRY AND HIGH-TEMPERATURE GEOCHEMISTRY
Abstract
▪ Abstract The Re-Os isotope sytem, based on the long-lived β−transition of 187 Re to 187 Os, has matured to wide use in cosmochemistry and high-temperature geochemistry. The siderophilic/chalcophilic behavior of Re and Os is different from that of the elements that comprise most other long-lived radiogenic isotope systems. Magmatic iron meteorites (IIIAB, IIAB, IVA, and IVB) have Re-Os isochrons that indicate asteroidal core crystallization within the first 10–40 million years of Solar System evolution. Rocks from Earth's convecting mantle show generally chondritic Re/Os evolution throughout Earth history that is explained by the addition of highly siderophile elements to the mantle after core formation via late accretion. Oceanic basalts have Os-isotope systematics that improve the detailed geological interpretation of extant mantle components. Some portions of ancient subcontinental lithospheric mantle are severely depleted in Re and have correspondingly subchondritic 187 Os/188 Os, indicating long-term isolation from the convecting mantle during the Archean-Proterozoic. Magmatic ore deposits have differences in initial Os isotopic composition traceable to the crustal vs mantle sources of the platinum-group elements and base metals.
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Citations
Cites
Mantle geochemistry: The message from oceanic volcanism
Hofmann, A. W. (1997) · Nature · doi:10.1038/385219a0 · Cited by 2,782
Formation of an Archaean continent
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Cited by
Griffin, W. L., Pearson, N. J., Belousova, E., Jackson, S. E., van Achterbergh, E., O’Reilly, S. Y., & Shee, S. R. (2000) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(99)00343-9 · Cited by 3,385
Assessment of international reference materials for isotope-ratio analysis (IUPAC Technical Report)
Brand, W. A., Coplen, T. B., Vogl, J., Rosner, M., & Prohaska, T. (2014) · Pure and Applied Chemistry · doi:10.1515/pac-2013-1023 · Cited by 704
Recycled dehydrated lithosphere observed in plume-influenced mid-ocean-ridge basalt
Dixon, J. E., Leist, L., Langmuir, C., & Schilling, J.-G. (2002) · Nature · doi:10.1038/nature01215 · Cited by 523
Ancient, highly heterogeneous mantle beneath Gakkel ridge, Arctic Ocean
Liu, C.-Z., Snow, J. E., Hellebrand, E., Brügmann, G., von der Handt, A., Büchl, A., & Hofmann, A. W. (2008) · Nature · doi:10.1038/nature06688 · Cited by 342
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Metadata
- Authors
- Shirey, S. B., & Walker, R. J.
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 1998-05
- Volume
- 26
- Issue
- 1
- Pages
- 423-500
- ISSN
- 0084-6597 (ISSN-L)
- 1545-4495
- OpenAlex
- W2166632770
- Cited by
- 975
- References
- 2
- FWCI
- 4.16
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: THE R e-O s ISOTOPE SYSTEM IN COSMOCHEMISTRY AND HIGH-TEMPERATURE GEOCHEMISTRY. https://app.cochat.ai/papers/10.1146/annurev.earth.26.1.423
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- Shirey, S. B., & Walker, R. J. (1998). THE R e-O s ISOTOPE SYSTEM IN COSMOCHEMISTRY AND HIGH-TEMPERATURE GEOCHEMISTRY. Annual Review of Earth and Planetary Sciences. https://doi.org/10.1146/annurev.earth.26.1.423
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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