Muscovite mica is a common rock-forming mineral that occurs in granites, pegmatites, and metamorphic rocks. It has a sheet-like structure and ranges in color from colorless to various shades of brown, green, and red. Muscovite is the most prevalent mica and is mined commercially, with major deposits located in India, Brazil, and the United States. It has a variety of industrial and commercial uses such as insulation, construction, and paint fillers.
2. What is Mica?
Mica is a generic term applied to a group of rock-forming complex
aluminosilicate minerals having a sheet or plate like structure with varying
chemical composition and physical properties.
3. Types Of Mica
Of the nine common varieties in the mica group of minerals, the two principal
classes of Mica types of commercial importance are
Muscovite : K Al2 (Al Si3 O10 )(OH) 2 and
Phlogopite : K Mg3 (Al Si3O10 )(OH) 2
4. Muscovite Mica
It is a hydrous potassium aluminium silicate with a predominance of
potassium. It ranges from colourless through browns to greens or reds.
5. Phlogopite Mica
It is a hydrous magnesium aluminium silicate with a predominance of
magnesium. It is commonly called as “Amber Mica” which varies in colour
from light silver to dark brown or amber.
6. Occurence
Muscovite is the most common mica, found in Granites,
Pegmatites, Gneisses, and Schists, and as a contact
metamorphic rock or as a secondary mineral resulting
from the alteration of Topaz, Feldspar, Kyanite, etc.
In Pegmatites, it is often found in immense sheets that
are commercially valuable.
7. Exploration and exploitation is successfully carried
by means of systematic vertical shaft and open cast
mining. The principal muscovite mica deposits are
chiefly found in the States of Jharkhand, Rajasthan
and Andhra Pradesh.
Jharkhand (formerly Bihar State) which produces the
world's finest muscovite mica well known throughout
the globe
8.
9.
10. Muscovite
Mica may be
divided into two
color groups :
RUBY MUSCOVITE
GREEN MUSCOVITE
11. Ruby Muscovite
Colour ranges from an almost white
through pink to a light ruby and
into shades of brownish ruby and
brown. It is produced in the Indian
States of Jharkhand and Rajasthan.
12. Green Muscovite
Ranges from light to pale green through yellowish
and olive green to a dark green. It is produced
in the Indian State of Andhra Pradesh.
14. Colour:White to colorless, silvery-white, and tinged various colors by
impurities.
Streak:White
Hardness (Mohs): 2½
15. Cleavage:Perfect
Perfect on {001}.
Fracture:Micaceous
Crystal System: Monoclinic with
a = 5.199Å, b = 9.027Å, c = 20.106Å
β = 95.78°
16. DISTINGUISHING SIMILAR MINERALS
Chlorite and Margarite - Not as elastic as Muscovite.
Biotite, Phlogopite - Usually darker in color, otherwise very difficult to
distinguish.
Lepidolite - Very difficult to distinguish from pink Muscovite.
Gypsum - Cannot be peeled into micaceous sheets, crystals usually
differently shaped.
22. Muscovite is an extremely common mineral, some bright yellow and others with perfect
star formations, come from the famous pegmatite localites in the Doce and
Jequitinhonha Valleys in Minas Gerais Brazil. Specific localities include Divino das
Laranjeiras ("stars"),Galileia, Governador Valadares, Conselheiro Pena, Jaguaracu,
Aracuai, and Coronel Murta. Beautiful yellow Muscovite comes from the Davib Ost Farm,
Karibib, Erongo, Namibia. Fine Muscovite plates, often associated with
valuable pegmatitegemstones, come from the Shigar Valley and Skardu District in
Northern Pakistan. Nellore, India, is famous for its Muscovite mines which have produced
some of the worlds largest mica sheets. Xuebaoding Mountain, Pingwu, in Sichuan
Province, China, provides excellent Aquamarine and Scheelite that are associated with
beautiful Muscovite plates.
In the U.S., Muscovite is fairly common in the pegmatites of San Diego county, including
Pala and Ramona. Rare Muscovitepseudomorphs after Tourmaline come from the Willow
Spring Ranch, Oracle, Pinal Co., Arizona. A bright pink, lithium-rich variety comes from the
Harding Mine, Taos Co., New Mexico; and gemmy green crystals from Lincoln Co., North
Carolina. Other important localties include Mt Antero, Chaffee Co., Colorado; the
Diamond Mica Mine, Keystone, Pennington Co., South Dakota; Shelby, Cleveland Co.,
North Carolina; and Bedford, Westchester Co., New York.
New England contains some important Muscovite in its famous pegmatites, specifically at
Middlesex Co., Connecticut (East Hampton, Haddam, and Portland); Grafton Co., New
Hampshire (the Palermo No. 1 Mine, Groton; and the Ruggles Mine, Grafton); Mt. Apatite,
Auburn, Androscoggin Co., Maine; and Greenwood and Newry, Oxford Co., Maine.
Editor's Notes
Crystals of Mica are characterised by highly perfect basal cleavage in the direction of large surfaces permitting it to split or delaminate into extremely thin and flat films.
Types of Mica Anandite, Annite, Biotite, Celadonite, Roscoelite, Illite
Phlogopite from Kiran, Kokcha Valley, Badakhshan, AfghanistanLazurite
Muscovy Glass, Cat Silver, and Lapis Specularis (stone mirror); The name muscovite comes from Muscovy-glass, a name
given to the mineral in Elizabethan England due to its use in medieval Russia as a cheaper alternative to glass in windows.
Muscovite Mica is transparent and harder than Phlogopite Mica having more widespread availability.
Muscovite Mica from Bancroft, Ontario CANADA
Transparency is less than Muscovite Mica and its films are a bit cloudy. Phlogopite Mica is softer than Muscovite Mica but has greater heat resistance and thermal durability.
In igneous rocks it is a primary mineral that is especially common in granitic rocks. In granite pegmatites muscovite is often found in large crystals with a pseudohexagonal outline. These crystals are called "books" because they can be split into paper-thin sheets. Muscovite rarely occurs in igneous rocks of intermediate, mafic and ultramafic composition.
Muscovite can form during the regional metamorphism of argillaceous rocks. The heat and pressure of metamorphism transforms clay minerals into tiny grains of mica which enlarge as metamorphism progresses. Muscovite can occur as isolated grains in schist and gneiss or it can be abundant enough that the rocks are called "mica schist" or "micaceous gneiss".
Sheets of muscovite 5×3 m have been found in Nellore, India.
A pegmatite is a holocrystalline, intrusive igneous rock composed of interlocking phaneritic crystals usually larger than 2.5 cm in size; such rocks are referred to aspegmatitic. Most pegmatites are composed of quartz, feldspar and mica, having a similar basic composition as granite.
COMMON MINERAL ASSOCIATIONS - Albite, Quartz, Microcline, Almandine, Spodumene"argillaceous" is also used to define rocks in which clay minerals are a secondary but significant component.
Vast exploitable reserves are found chiefly in India which produces and markets over 80% of the total global output of Muscovite Mica.
The green, chromium-rich variety is called fuchsite; (mariposite)- cr rich
Both Ruby Mica and Green Mica are equally suitable under normal working conditions.Fuschite, Alurgite, Mariposite, Schernikite , Sericite, Star Muscovite
Still, Ruby Mica is generally preferred since at elevated temperatures Green Mica displays erratic electrical characteristics. The structure of Green Muscovite is stable but less perfect as compared to Ruby Muscovite. Moreover, Ruby Muscovite is harder than Green Muscovite having excellent cleavage permitting it to be split into the thinnest desired film without the risk of cracking.
It is a Phylosilicates minerals, i.e they have each set of tetrahedrons surrounded by three oxygen atoms, forming a sheet like structure.
Crystals are in thick flakes, micaceous masses and groupings, and in tabular, foliated, flaky, and scalyforms.
Tenacity:Elastic
It has a highly-perfect basal cleavage yielding remarkably-thin laminæ (sheets) which are often highly elastic.
Muscovite is in demand for the manufacture of fireproofing and insulating materials and to some extent as a lubricant.