Ion microprobe Al–Mg dating of single plagioclase grains in an Efremovka chondrule
Author:
Affiliation:
1. Atmosphere and Ocean Research Institute, The University of Tokyo
2. Department of Earth and Planetary Sciences, The University of Tokyo
Publisher
Geochemical Society of Japan
Subject
Geochemistry and Petrology,Geophysics
Link
https://www.jstage.jst.go.jp/article/geochemj/48/2/48_2.0294/_pdf
Reference31 articles.
1. Amelin, Y., Krot, A. N., Hutcheon, I. D. and Ulyanov, A. A. (2002) Lead isotopic ages of chondrules and calcium–aluminum-rich inclusions. Science 297, 1678-1683.
2. Dodson, M. H. (1973) Closure temperature in cooling geochronological and petrological systems. Cont. Mineral. Petrol. 40, 259-274.
3. Goswami, J. N., Srinivasan, G. and Ulyanov, A. A. (1994) Ion microprobe studies of Efremovka CAIs: I. Magnesium isotope composition. Geochim. Cosmochim. Acta 58, 431-447.
4. Harrison, K. P. and Grimm, R. E. (2010) Thermal constraints on the early history of the H-chondrite parent body reconsidered. Geochim. Cosmochim. Acta 74, 5410-5423.
5. Hutcheon, I. D., Marhas, K. K., Krot, A. N., Goswami, J. N. and Jones, R. H. (2009) 26Al in plagioclase-rich chondrules in carbonaceous chondrites: evidence for an extended duration of chondrule formation. Geochim. Cosmochim. Acta 73, 5080-5099.
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