New finding of paragonite–clinozoisite association in garnet from the type locality of Sanbagawa belt (Kanto Mountains, Japan)

Author:

MIYASHITA Atsushi1

Affiliation:

1. Seikei High School

Publisher

Japan Association of Mineralogical Sciences

Subject

Geology,Geophysics

Reference26 articles.

1. Aoki, K., Itaya, T., Shibuya, T., Masago, H., Nishizawa, M., Terabayashi, M., Omori, S., Yokoyama, T., Takahara, N., Sano, Y. and Maruyama, S. (2008) The youngest blueschist belt in SW Japan: implication for the exhumation of the Cretaceous Sanbagawa high–P/T metamorphic belt. Journal of Metamorphic Geology 26, 583–602.

2. Aoki, K., Maruyama, S., Isozaki, Y., Otoh, S. and Yanai, S. (2011) Recognition of the Shimanto HP metamorphic belt within the traditional Sanbagawa HP metamorphic belt: New perspectives of the Cretaceous–Paleogene tectonics in Japan. Journal of Asian Earth Science, 42, 355–369.

3. Banno, S. and Sakai, C. (1989) Geology and metamorphic evolution of the Sanbagawa belt. In Evolution of Metamorphic Belts (Daly, J.S., Cliff, R.A., and Yardley, B.W.D. Eds.). Proceedings of the 1987 Joint Meeting of the Metamorphic Studies Group and IGCP Project 235: Geological Society, London, Special Publication, 43, 519–532.

4. Franz, G. and Althaus, E.K. (1977) The stability relations of paragenesis paragonite–zoisite–quartz. Neues Jahrbuch für Mineralogie–Abhandlungen, 130, 159–167.

5. Goto, A., Higashino, T. and Sakai, C. (1996) XRF analyses of Sanbagawa pelitic schists in central Shikoku, Japan. Memoirs of Faculty of Science, Kyoto University, Series of Geology and Mineralogy, 58, 1–19.

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1. Low-angle structural boundaries in northern marginal area of the Kanto Mountains;The Journal of the Geological Society of Japan;2016-07-15

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