-
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...
-
subgroup (part of the kaolinite-serpentine
group in the
category of
phyllosilicates) are greenish, brownish, or
spotted minerals commonly found in serpentinite...
-
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;...
-
highly porous interior, and
suggesting a
composition containing mainly phyllosilicates and
other minerals known from Mars,
point toward an
origin of Phobos...
-
monoclinic crystals show
micaceous cleavage, a
distinguished property of
phyllosilicates, and fuse with difficulty.
Serpentinite rocks that
consist of mostly...
- a yellow, greenish, or reddish-brown
member of the mica
family of
phyllosilicates. It is also
known as
magnesium mica.
Phlogopite is the
magnesium endmember...
- from mud that is a mix of
flakes of clay
minerals (hydrous
aluminium phyllosilicates, e.g., kaolin, Al2Si2O5(OH)4) and tiny
fragments (silt-sized particles)...
-
Montmorillonite is a very soft
phyllosilicate group of
minerals that form when they
precipitate from
water solution as
microscopic crystals,
known as clay...
