Geochronology and REE geochemistry of zircon and garnet in pelitic gneisses from the Higo metamorphic terrane, Kyushu, Japan: Constraints on the timing of high–temperature metamorphism
Author:
Affiliation:
1. Graduate School of Integrated Sciences for Global Society, Kyushu University
2. Division of Earth Sciences, Faculty of Social and Cultural Studies, Kyushu University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/114/2/114_181115/_pdf
Reference31 articles.
1. Adachi, T., Osanai, Y., Nakano, N. and Owada, M. (2012) LA–ICP–MS U–Pb Zrn and FE–EPMA U–Th–Pb monazite dating of pelitic granulites from the Mt. Ukidake area, Sefuri Mountains, northern Kyushu. The Journal of Geological Society of Japan, 118, 29–52.
2. Dunkley, D., Suzuki, K., Hokada, T. and Kusiak, M. (2008) Constrasting ages between isotopic chronometers in granulites: Monazite dating and metamorphism in the Higo Complex, Japan. Gondwana Research, 14, 623–643.
3. Fraser, G., Ellis, D. and Eggins, S. (1997) Zirconium abundance in granulite–facies minerals, with implications for zircon geochronology in high–grade rocks. Geology, 25, 607–610.
4. Hamamoto, T., Osanai, Y. and Kagami, H. (1999) Sm–Nd, Rb–Sr and K–Ar geochronology of Higo metamorphic terrane, west–central Kyushu, Japan. The Island Arc, 8, 323–334.
5. Harley, S.L. (2002) Zircon–garnet REE distribution patterns and the behaviour of Zrn during UHT metamorphism. Programme with Abstracts, International Mineralogical Association 18, Edinburgh, 236.
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