-
rhodonite Inosilicate with
cyclic branched 8-periodic chain,
pellyite Phyllosilicates (from Gr**** φύλλον phýllon 'leaf'), or
sheet silicates, form parallel...
- Clay
minerals are
hydrous aluminium phyllosilicates (e.g. kaolin, Al2Si2O5(OH)4),
sometimes with
variable amounts of iron, magnesium,
alkali metals, alkaline...
-
whereas double-chain
silicates have two or
three shared corners.
Phyllosilicates Have a
sheet structure which requires three shared oxygens; in the...
-
Vermiculite is a
hydrous phyllosilicate mineral which undergoes significant expansion when heated.
Exfoliation occurs when the
mineral is
heated sufficiently;...
-
subgroup (part of the kaolinite-serpentine
group in the
category of
phyllosilicates) are greenish, brownish, or
spotted minerals commonly found in serpentinite...
-
Montmorillonite is a very soft
phyllosilicate group of
minerals that form when they
precipitate from
water solution as
microscopic crystals,
known as clay...
- the Rock
Forming Minerals, Longman, ISBN 0-582-44210-9. "Mineralogy:
Phyllosilicates".
Colgate University. 1997.
Archived from the
original on 19 September...
-
Indistinct LL6
Melted LL7
Carbonaceous chondrites Ivuna Phyllosilicates,
Magnetite CI
Mighei Phyllosilicates,
Olivine CM1–CM2
Vigarano Olivines rich in Fe, Ca...
- The name
apophyllite refers to a
specific group of
phyllosilicates, a
class of minerals. Originally, the
group name
referred to a
specific mineral, but...
- is a soft,
fibrous silicate mineral in the
serpentine subgroup of
phyllosilicates; as such, it is
distinct from
other asbestiform minerals in the amphibole...
