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Evidence for the stability of the potential nuclear waste host, sphene, over geological time, from uranium-lead ages and uranium-series measurements
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The closure temperature for sphene is generally considered to be about 500 to 550 °C.
“The closure temperature for sphene is generally considered to be about 500 to 550~ (e.g., Mattinson 1978;Gascoyne 1986).”
From U-Pb geochronology of the Grenville Orogen of Ontario and New York: constraints on ancient crustal tectonics (1993) · cites this paper as Gascoyne 1986
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Research works printed but not linked: 39
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Cited by
Sorted by citations
Mezger, K., Essene, E. J., van der Pluijm, B. A., & Halliday, A. N. (1993) · Contributions to Mineralogy and Petrology · doi:10.1007/bf00307862 · Cited by 166
Metadata
- Authors
- Gascoyne, M.
- Venue
- Applied Geochemistry
- Publisher
- Elsevier BV
- Published
- 1986-03
- Volume
- 1
- Issue
- 2
- Pages
- 199-210
- ISSN
- 0883-2927
- Cited by
- 32
- References
- 0
- Language
- en
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