PHLOGOPITE
, a See also:mineral belonging to the See also:group of micas (q.v.)
.
It is a See also:magnesium See also:mica, differing from See also:biotite in containing only a little See also:iron; the chemical See also:formula is [H,K,(MgF)]3Mg3Al(SiOi)3
.
It crystallizes in the See also:monoclinic See also:system, but the crystals are roughly See also:developed
.
There is a perfect cleavage parallel to the basal See also:plane; the cleavage flakes are not quite so elastic as those of See also:muscovite
.
Sometimes it is quite colourless and transparent, but usually of a characteristic yellowish-See also:- BROWN
- BROWN, CHARLES BROCKDEN (1771-181o)
- BROWN, FORD MADOX (1821-1893)
- BROWN, FRANCIS (1849- )
- BROWN, GEORGE (1818-188o)
- BROWN, HENRY KIRKE (1814-1886)
- BROWN, JACOB (1775–1828)
- BROWN, JOHN (1715–1766)
- BROWN, JOHN (1722-1787)
- BROWN, JOHN (1735–1788)
- BROWN, JOHN (1784–1858)
- BROWN, JOHN (1800-1859)
- BROWN, JOHN (1810—1882)
- BROWN, JOHN GEORGE (1831— )
- BROWN, ROBERT (1773-1858)
- BROWN, SAMUEL MORISON (1817—1856)
- BROWN, SIR GEORGE (1790-1865)
- BROWN, SIR JOHN (1816-1896)
- BROWN, SIR WILLIAM, BART
- BROWN, THOMAS (1663-1704)
- BROWN, THOMAS (1778-1820)
- BROWN, THOMAS EDWARD (1830-1897)
- BROWN, WILLIAM LAURENCE (1755–1830)
brown See also:colour, and often with a silvery lustre on the cleavage surfaces, hence the See also:trade name " See also:silver See also:amber mica " for some varieties
.
The name phlogopite is from Gr
.
4 Xoynnros (fiery-looking), the mineral being sometimes brownish-red and coppery in See also:appearance
.
The hardness is 22-3, and the specific gravity 2.78-2.85
.
The optic axial plane is parallel to the plane of symmetry and the axial See also:angle o°-lo°
.
Phlogopite occurs chiefly as scales and plates embedded in crystalline limestones of the Archean formation
.
The mica See also:mined in See also:Canada and See also:Ceylon is mainly phlogopite; and is largely used as an insulator for See also:electrical purposes
.
In Canada it occurs with See also:apatite in See also:pyroxene rocks which are intrusive in Laurentian gneisses and crystalline limestones, the See also:principal See also:mining See also:district being in See also:Ottawa See also:county in See also:Quebec and near See also:Burgess in See also:Lanark county, See also:Ontario
.
In Ceylon, the mineral forms irregular See also:veins, rarely exceeding one or two feet in width, traversing See also:granulite, especially near the coptact of this See also:rock with crystalline
See also:limestone
.
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.
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.
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