A matter of time: The importance of the duration of UHT metamorphism
Author:
Affiliation:
1. School of Geosciences, University of Edinburgh
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/111/2/111_160128/_pdf
Reference116 articles.
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2. Ashwal, L.D, Tucker, R.D and Zinner, E.K. (1999) Slow cooling of deep crustal granulitesand Pb–loss in zircon. Geochimica et Cosmochimica Acta, 63, 2839–2851.
3. Baba, S., Dunkley, D.J., Hokada, T., Horie, K., Suzuki, K. and Shiraishi, K. (2012) New SHRIMP U–Pb zircon ages and CHIME monazite ages from South Harris granulites, Lewisian Complex, NW Scotland: Implications for two stages of zircon formation during Palaeoproterozoic UHT metamorphism. Precambrian Research, 200–203, 104–128.
4. Baldwin, J.A., Brown, M. and Schmitz, M.D. (2007) First application of titanium–in–zircon thermometry to ultrahigh–temperature metamorphism. Geology, 35, 295–298.
5. Baldwin, J.A. and Brown, M. (2008) Age and duration of ultrahigh–temperature metamorphism in the Anápolis–Itauçu Complex, Southern Brasilia Belt, central Brazil — constraints from U–Pb geochronology, mineral rare earth element chemistry and trace–element thermometry. Journal of Metamorphic Geology, 26, 213–233.
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