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UPb ages for sphene in a contact metamorphic zone
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The closure temperature for sphene is about 550 to 650 °C depending on the grain size.
“A comparison of sphene ages with ages of other minerals in the Adirondacks and reevaluation of sphene data from the contact aureole of the Duluth Gabbro (Hanson et al. 1971) led to the suggestion that the closure temperature for sphene is about 550 to 650 ~ depending on the grain size (Mezger et al. 1991a).”
From U-Pb geochronology of the Grenville Orogen of Ontario and New York: constraints on ancient crustal tectonics (1993) · cites this paper as Hanson et al. 1971
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No references could be resolved yet.
Research works printed but not linked: 13
- Tilton, 1968, Sphene: uranium-lead ages, Science, 159, 1458, 10.1126/science.159.3822.1458 · DOI
- Hanson, 1967, Kinetic studies in contact metamorphic zones, Geochim. Cosmochim. Acta, 31, 1119, 10.1016/S0016-7037(67)80053-X · DOI
- Green, 1970, Lower Precambrian rocks of the Gabbro Lake Quadrangle, northeastern Minnesota, Minnesota Geological Survey SP-13, 99
- E. Catanzaro and G. Hanson, UPb ages for sphene from early Precabrian igneous rocks in northeastern Minnesota and northwestern Ontario, Can. J. Earth Science (in press).
- Hanson, 1971, KAr ages of mafic dikes and evidence for low-grade metamorphism in northeastern Minnesota, Geol. Soc. Am. Bull., 82, 1107, 10.1130/0016-7606(1971)82[1107:KAOMDA]2.0.CO;2 · DOI
- Davis, 1968, Some effects of contact metamorphism on zircon ages, Earth Planet. Sci. Letters, 5, 27, 10.1016/S0012-821X(68)80006-8 · DOI
- Goldich, 1961, The Precambrian geology and geochronology of Minnesota, Minnesota Geol. Surv. Bull., 41, 193
- Phinney, 1969, The Duluth complex in the Gabbro Lake Quadrangle, Minnesota, Minnesota Geol. Surv. Rep. of Investigation, 9, 20
- Jaeger, 1957, The temperature in the neighborhood of a a cooling intrusive sheet, Am. J. Sci., 255, 306, 10.2475/ajs.255.4.306 · DOI
- Perry, 1966, Quartz and magnetite: O18/O16 fractionation profile from the metamorphosed Biwabik iron formation, Science, 153, 528, 10.1126/science.153.3735.528 · DOI
- Hanson, 1968, KAr ages for hornblende from granites and gneisses and for basaltic intrusives in Minnesota, Minnesota Geol. Surv. Rep. of Investigation, 8, 20
- Krogh, 1969, Old isotopic ages in the northwestern Grenville province, Ontario, Geol. Assoc. Canada, Spec. Paper, 5, 189
- Wetherill, 1956, Discordant uranium-lead ages, Trans. Am. Geophys. Un., 37, 320, 10.1029/TR037i003p00320 · DOI
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
- Hanson, G. N., Catanzaro, E. J., & Anderson, D. H.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 1971-10
- Volume
- 12
- Issue
- 2
- Pages
- 231-237
- ISSN
- 0012-821X
- Cited by
- 35
- References
- 0
- Language
- en
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