RECOMMENDED NOMENCLATURE FOR ZEOLITE MINERALS - REPORT OF THE SUBCOMMITTEE ON ZEOLITES OF THE INTERNATIONAL MINERALOGICAL ASSOCIATION, COMMISSION ON NEW MINERALS AND MINERAL NAMES
Ds. Coombs et al., RECOMMENDED NOMENCLATURE FOR ZEOLITE MINERALS - REPORT OF THE SUBCOMMITTEE ON ZEOLITES OF THE INTERNATIONAL MINERALOGICAL ASSOCIATION, COMMISSION ON NEW MINERALS AND MINERAL NAMES, European journal of mineralogy, 10(5), 1998, pp. 1037-1081
This report embodies recommendations on zeolite nomenclature approved
by the International Mineralogical Association Commission on New Miner
als and Mineral Names. In a working definition of a zeolite mineral us
ed for this review, structures containing an interrupted framework of
tetrahedra are accepted where other zeolitic properties prevail, and c
omplete substitution by elements other than Si and Al is allowed. Sepa
rate species are recognized in topologically distinctive compositional
series in which different extra-framework cations are the most abunda
nt in atomic proportions. To name these, the appropriate chemical symb
ol is attached by a hyphen to the series name as a suffix, except for
the names harmotome, pollucite and wairakite in the phillipsite and an
alcime series. Differences in space-group symmetry and in order-disord
er relationships in zeolites having the same topologically distinctive
framework do not in general provide adequate grounds for recognition
of separate species. Zeolite species are not to be distinguished solel
y on Si:Al ratio except for heulandite (Si:Al < 4.0) and clinoptilolit
e (Si:Al greater than or equal to 4.0). Dehydration, partial hydration
and over-hydration are not sufficient grounds for the recognition of
separate species of zeolites. Use of the term ''ideal formula'' should
be avoided in referring to a simplified or averaged formula of zeolit
e. Newly recognized species in compositional series are as follows: br
ewsterite-Sr, -Ba; chabazite-Ca, -Na, -K; clinoptilolite-K, -Na, -Ca;
dachiardite-Ca, -Na; erionite-Na, -K, -Ca; faujasite-Na, -Ca, -Mg; fer
rierite-Mg, -K, -Na; gmelinite-Na, -Ca, -K; heulandite-Ca, -Na, -K, -S
r; levyne-Ca, -Na; paulingite-K, -Ca; phillipsite-Na, -Ca, -K; stilbit
e-Ca, -Na. Key references, type locality, origin of name, chemical dat
a, IZA structure-type symbols, space-group symmetry, unit-cell dimensi
ons, and comments on structure are listed for 13 compositional series,
82 accepted zeolite mineral species, and three of doubtful status. He
rschelite, leonhardite, svetlozarite and wellsite are discredited as m
ineral species names. Obsolete and discredited names are listed.