Dalyite (K2ZrSi6O15) and Zektzerite (LiNaZrSi6O15) in Aegirine-bearing Albitite from Iwagi Islet, SW Japan

Author:

IMAOKA Teruyoshi1,AKITA Sachiho2,NAGASHIMA Mariko1ORCID

Affiliation:

1. Graduate School of Science and Technology for Innovation, Yamaguchi University

2. Asahi Consultant Co., Ltd.

Publisher

Tokyo Geographical Society

Subject

Earth-Surface Processes,Geology,Geophysics,Geography, Planning and Development,Global and Planetary Change

Reference34 articles.

1. Andrade, M.B., Doell, D., Downs, R. and Yang, H. (2013): Redetermination of katayamalite, KLi3Ca7Ti2(SiO3)12(OH)2. Acta Crystallographica, E69, i41.

2. Armbruster, T. and Oberhänsli, R. (1988): Crystal chemistry of double-ring silicates: structures of sugilite and brannockite. American Mineralogist, 73, 595-600.

3. Boulvais, P., Ruffet, G., Cornichet, J. and Mermet, M. (2007): Cretaceous albitization and dequartzification of Hercynian peraluminous granites in the Salvezines Massif (French Pyrenees). Lithos, 93, 89-106.

4. Caruba, R., Baumer, A. and Turco, G. (1970): Première synthèse hydrothermale de la dalyite K2ZrSi6O15. Données radiocrystallographiques. C.R. Academie des Sciences, Paris 270, sér. D, 2741-2744.

5. Cathelineau, M. (1986): The hydrothermal alkali metasomatism effects on granitic rocks: Quartz dissolution and related subsolidus changes. Journal of Petrology, 27, 945-965.

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