Mineralogical heterogeneity of UHP garnet peridotite in the Moldanubian Zone of the Bohemian Massif (Nové Dvory, Czech Republic)

Author:

MURIUKI Juliah1,NAKAMURA Daisuke1,HIRAJIMA Takao2,SVOJTKA Martin3

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

Reference61 articles.

1. Ackerman, L., Bizimis, M., Haluzová, E., Sláma, J., et al (2016) Re–Os and Lu–Hf isotopic constraints on the formation and age of mantle pyroxenites from the Bohemian Massif. Lithos, 256, 197–210.

2. Ackerson, M.R., Tailby, N., Watson, E.B. and Spear, F.S. (2013) Variations in Ti coordination and concentration in garnet in response to temperature, pressure and composition. In abstracts of American Geophysical Union Fall Meeting, the American Geophysical Union, Washington D.C., U.S.A.

3. Altherr, R. and Kalt, A. (1996) Metamorphic evolution of ultrahigh–pressure garnet peridotites from the Variscan Vosges Mts. (France). Chemical Geology, 134, 27–47.

4. Arai, S. (1984) Pressure–temperature dependent compositional variation of phlogopitic micas in upper mantle peridotites. Contributions to Mineralogy and Petrology, 87, 260–264.

5. Baba, T., Nakamura, D., Svojtka, M. and Hirajima, T. (2015) Texture and Pressure–temperature estimation of garnet peridotite occurring in the Bohemian Massif, Czech Republic. The Abstracts with Program 2016 Annual Meeting of Japan Association of Mineralogical Sciences, Japan, R8–P15.

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