A “Calcian Analcime” in Ophiolite from Sugasima, Mié Prefecture, Japan
Author:
Affiliation:
1. Section of Geology and Mineralogy, Chichibu Museum of Natural History
2. Department of Geology, National Science Museum
Publisher
Japan Academy
Subject
General Medicine
Link
https://www.jstage.jst.go.jp/article/pjab1945/43/9/43_9_889/_pdf
Reference18 articles.
1. Beattie, I. R.: The structure of analcime and ion-exchange forms of analcime. Acta Cryst., 7, 357-359 (1954).
2. Coombs, D. S.: X-ray observations on wairakite and non-cubic analcime. Mineral. Mag., 30, 699-708 (1955).
3. Coombs, D. S.: Lower grade mineral facies in New Zealand. Rept. 21st Internat. Geol. Congr., Part 13 (petrographic province, igneous and metamorphic rocks), 339-351, Copenhagen (1960).
4. Coombs, D. S.: Some recent work on the lower grade of metamorphism. Austr. J. Sci., 24, 203-215 (1961).
5. Coombs, D. S., Ellis, A. J., Fyfe, W. S., and Taylor, A. M.: The zeolite facies, with comments on the interpretation of hydrothermal syntheses. Geoch. Cosmoch. Acta, 17, 53-107 (1959).
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1. A consideration on the wairakite–analcime series.—Is valid a new mineral name for sodium analogue of monoclinic wairakite?—;Mineralogical Journal;1976
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