Recommended nomenclature for zeolite minerals: report of the subcommittee on zeolites of the International Mineralogical Association, Commission on new Minerals and Mineral names

Canadian Mineralogist

Volumn 35, Issue 6, 1997, Pages 1571-1606

  Coombs, Douglas S ^a   Alberti, Alberto ^b   Armbruster, Thomas ^c   Artioli, Gilberto ^d   Colella, Carmine ^e   Galli, Ermanno ^f   Grice, Joel D ^g   Liebau, Friedrich ^h   Mandarino, Joseph A ⁱ   Minato, Hideo ^j   Nickel, Ernest H ^k   Passaglia, Elio ^f   Peacor, Donald R ^l   Quartieri, Simona ^f   Rinaldi, Romano ^m   Ross, Malcolm ⁿ   Sheppard, Richard A ^o   Tillmanns, Ekkehart ^p   Vezzalini, Giovanna ^f  

^a UNIVERSITY OF OTAGO   (New Zealand)

^b UNIVERSITY OF FERRARA   (Italy)

^c UNIVERSITY OF BERN   (Switzerland)

^d UNIVERSITY OF MILAN   (Italy)

^e UNIVERSITY OF NAPLES FEDERICO II   (Italy)

^f UNIVERSITY OF MODENA AND REGGIO EMILIA   (Italy)

^g CANADIAN MUSEUM OF NATURE   (Canada)

^h UNIVERSITY OF KIEL   (Germany)

ⁱ DEPARTMENT OF NATURAL HISTORY   (Canada)

^j CSIRO ^*  (Japan)

^k CSIRO   (Australia)

^l UNIVERSITY OF MICHIGAN   (United States)

^m UNIVERSITY OF PERUGIA   (Italy)

ⁿ U S GEOLOGICAL SURVEY   (United States)

^o DENVER FEDERAL CENTER   (United States)

^p UNIVERSITY OF VIENNA   (Austria)

more..

Author keywords

[No Author keywords available]

Indexed keywords

CRYSTALLOGRAPHY; NUMERICAL NOMENCLATURE; ZEOLITE;

EID: 13144257683     PISSN: 00084476     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (22)

1. AKIZUKI, M. (1985): The origin of sector twinning in harmotome. Am. Mineral. 70, 822-828.
2. _ (1986): Al-Si ordering and twinning in edingtonite. Am. Mineral. 71, 1510-1514.
3. _ (1987a): Crystal symmetry and order-disorder structure of brewsterite. Am. Mineral. 72, 645-648.
4. _ (1987b): An explanation of optical variation in yugawaralite. Mineral. Mag. 51, 615-620.
5. VAUGHAN, P.A. (1966): The crystal structure of the zeolite ferrierite. Acta Crystallogr. 21, 983-990.
6. VEZZALINI, G. (1984): A refinement of Elba dachiardite: opposite acentric domains simulating a centric structure. Z. Kristallogr. 166, 63-71.
7. _, ARTIOLI, G. & QUARTIERI, S. (1992): The crystal chemistry of cowlesite. Mineral. Mag. 56, 575-579.
8. _ & OBERTI, R. (1984): The crystal chemistry of gismondines: the non-existence of K-rich gismondines. Bull. Minéral. 107, 805-812.
9. _, QUARTIERI, S. & GALLI, E. (1996): Relazioni strutturali nelle zeoliti con topologia CHA alla luce del ritrovamento di una Ca-willhendersonite. XXVI Congresso Nazionale della Associazione Italiana di Cristallografia (Alessandria), 91 (abstr.).
10. _, _ & _ (1997a): Occurrence and crystal structure of a Ca-pure willhendersonite. Zeolites 19, 75-79.
11. _, _, _, ALBERTI, A., CRUCIANI, G. & KVICK, Å. (1997b): Crystal structure of the zeolite mutinaite, the natural analogue of ZSM-5. Zeolites 19, 323-325.
12. _, _ & PASSAGLIA, E. (1990): Crystal structure of a K-rich natural gmelinite and comparison with the other refined gmelinite samples. Neues Jahrb. Mineral., Monatsh., 504-516.
13. VILLARROEL, H.S. (1983): Sobre la existencia de otras variedades de estellerita y una forma de reconocerlas. Anais Academia Brasileira de Ciencias 55, 87-91.
14. WALKER, G.P.L. (1962): Garronite, a new zeolite, from Ireland and Iceland. Mineral. Mag. 33, 173-186.
15. 2O, a new mineral species: mineral data and crystal structure. Eur. J. Mineral. 4, 1275-1283.
16. WENK, H.-R. (1973): The structure of wenkite. Z. Kristallogr. 137, 113-126.
17. WHITE, J.S. & ERD, R.C. (1992): Kehoeite is not a valid species. Mineral. Mag. 56, 256-258.
18. WISE, W.S. (1982): New occurrence of faujasite in southeastern California. Am. Mineral. 67, 794-798.
19. _ & TSCHERNICH, R.W. (1975): Cowlesite, a new Ca-zeolite. Am. Mineral. 60, 951-956.
20. _ & _ (1976): Chemical composition of ferrierite. Am. Mineral. 61, 60-66.
21. WYART, J. (1938): Étude sur la leucite. Bull. Soc. fr. Minéral. 61, 228-238.
22. YANG, PING & ARMBRUSTER, T. (1996): (010) disorder, partial Si,Al ordering, and Ca distribution in triclinic (C1) epistilbite. Eur. J. Mineral. 8, 263-271.