Hugo
Strunz's mineral classification system is a chemical-structural
mineral
classification system. All minerals are apportioned into one
of ten classes according to their principal anionic constituents
(Elements, Sulfides and sulphosalts, Halides, Oxides,
Carbonates, Borates, Sulfates, Phosphates, arsenates and vanadates,
Silicates and finally organic compounds).
Each
of these ten classes is then broken down into divisions,
subdivisions
and groups, based on chemical composition and crystal
structure. Within each chemical group the minerals are further
subdivided into structural
families and
finally isostructural groups.
For
each isostructural group, a brief description of the structure
is
given and then minerals are listed
with the chemical formula, crystal system, space group and
cell parameters. A simple alphanumeric coding system is applied
to
the various categories. This coding system has intentional
gaps that permit the insertion of new categories of minerals
yet to
be discovered without disrupting the general classification
scheme.