Maximum <i>P-T</i> conditions of felsic granulite occurring in the Zrcadlová Hut’ quarry of the Bohemian Massif, Czech Republic-Reference-Cited by-同舟云学术

Maximum <i>P-T</i> conditions of felsic granulite occurring in the Zrcadlová Hut’ quarry of the Bohemian Massif, Czech Republic

Published:2024 Issue:1 Volume:53 Page:n/a
ISSN:1345-630X
Container-title:Japanese Magazine of Mineralogical and Petrological Sciences
language:en
Short-container-title:Japanese Magazine of Mineralogical and Petrological Sciences

Author:

NAITO Mio¹,YAMANE Kensuke¹,NAKAMURA Daisuke¹

Affiliation:

1. Graduate School of Natural Science and Technology, Okayama University

Publisher

Japan Association of Mineralogical Sciences

Link

https://www.jstage.jst.go.jp/article/gkk/53/1/53_231216/_pdf

Reference40 articles.

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2. Arenas, R., Díez Fernández, R., Rubio Pascual, F.J., Sánchez Martínez, S., et al. (2016): The Galicia-Ossa-Morena Zone: Proposal for a new zone of the Iberian Massif. Variscan implications. Tectonophysics, 681, 135-143.

3. Bertrand, P. and Mercier, J.-C.C. (1985): The mutual solubility of coexisting ortho- and clinopyroxene: toward and absolute geothermometer for the natural system? Earth Planet. Sci. Lett., 76, 109-122.

4. Bohlen, S.R., Boettcher, A.L., Wall, V.J. and Clemens, J.D. (1983): Stability of phlogopite-quartz and sanidine-quartz: a model for melting in the lower crust. Contrib. Mineral. Petrol., 83, 270-277.

5. Carswell, D.A. (1991): Variscan high P-T metamorphism and uplift history in the Moldanubian zone of the Bohemian Massif in the Lower Austria. Eur. J. Mineral., 3, 323-342.