Pinkish colored epidotes found in a geothermal exploration well NB–1, Noboribetsu, Hokkaido-Reference-Cited by-同舟云学术

Pinkish colored epidotes found in a geothermal exploration well NB–1, Noboribetsu, Hokkaido

Published:2017 Issue:4 Volume:112 Page:147-158
ISSN:1345-6296
Container-title:Journal of Mineralogical and Petrological Sciences
language:en
Short-container-title:Journal of Mineralogical and Petrological Sciences

Author:

INOUE Atsuyuki¹,UTADA Minoru

Affiliation:

1. Department of Earth Sciences, Chiba University

Publisher

Japan Association of Mineralogical Sciences

Subject

Geology,Geophysics

Link

https://www.jstage.jst.go.jp/article/jmps/112/4/112_161229/_pdf

Reference30 articles.

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2. Barton, P.B., Jr. (1984) Redox reactions in hydrothermal fluids. In Fluid mineral equilibria in hydrothermal systems (Henley, R.W., Truesdell, A.H., Barton, P.B. Jr. and Whitney, J.A. Eds.). pp. 267, Reviews in Economic Geology, 1, Society of Economic Geologists, TX, 99–127.

3. Bonazzi, P. and Menchetti, S. (2004) Manganese in monoclinic members of the epidote group: piemontite and related minerals. In Epidote (Liebscher, A. and Franz, G. Eds.). pp. 628, Reviews in Mineralogy & Geochemistry, 56, Mineralogical Society of America and the Geochemical Society, Washington DC, 492–552.

4. Bourdelle, F., Parra, T., Chopin, C. and Beyssac, O. (2013) A new chlorite geothermometer for diagenetic to low–grade metamorphic conditions. Contributions to Mineralogy and Petrology, 165, 723–735.

5. Bourdelle, F. and Cathelineau, M. (2015) Low temperature chlorite geothermometry: a graphical representation based on a T–R²⁺–Si diagram. European Journal of Mineralogy, 27, 617–626.

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1. Compositional variation and zoning of epidote supergroup minerals in the Campi Flegrei geothermal field, Naples, Italy;European Journal of Mineralogy;2023-01-06

2. Application of chlorite thermometry to estimation of formation temperature and redox conditions;Clay Minerals;2018-06