Multiple origins of UHP eclogites in a garnet peridotite block (Nové Dvory, Czech Republic) and short duration of heating
Author:
Affiliation:
1. Graduate School of Natural Science and Technology, Okayama University
2. Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University
3. Institute of Geology of the Czech Academy of Sciences
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/117/1/117_220221/_pdf
Reference52 articles.
1. Aftalion, M., Bowes, D.R. and Vrána, S. (1989) Early Carboniferous U–Pb zircon age for garnetiferous, perpotassic granulites, Blanský les massif, Czechoslovakia. Neues Jahrbuch für Mineralgie Monatshefte, 4, 145–152.
2. Beard, B.L., Medaris, L.G., Johnson, C.M., Brueckner, K.H. and Mísař, Z. (1992) Petrogenesis of Variscan high–temperature Group A eclogites from the Moldanubian Zone of the Bohemian Massif, Czechoslovakia. Contributions to Mineralogy and Petrology, 111, 468–483.
3. Beyer, C., Frost, D.J. and Miyajima, N. (2015) Experimental calibration of a garnet–clinopyroxene geobarometer for mantle eclogites. Contributions to Mineralogy and Petrology, 169, DOI 10.1007/s00410-015-1113-z.
4. Carswell, D.A. and O’Brien, P.J. (1993) Thermobarometry and geotectonic significance of high–pressure granulites: examples from the Moldanubian Zone of the Bohemian Massif in Lower Austria. Journal of Petrology, 34, 427–459.
5. Cháb, J., Stráník, Z. and Eliáš, M. (2007) Geological map of Czech Republic 1:500000. Czech Geological Survey. Praha.
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