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</html>";s:4:"text";s:3644:"The crystal system of this mineral is monoclinic. This rock is composed of alkali feldspar and amphibole of the tremolite-actinolite series. Unusual pegmatite assemblage. Width of sample 7 cm. Phlogopite in glimmerite-carbonatite. 2. Biotite is one of the two most common members of the mica group. It is a common practice to distinguish between biotite and phlogopite like these two are mutually exclusive minerals with different compositions. Luumäki, Finland. The most characteristic property of these minerals is the perfect basal cleavage: Mica minerals have perfect basal cleavage which makes it easy to separate them into many thin folia. Kaatiala, Finland. Especially if the magma is contaminated by the material from pelitic crustal rocks. Hornblende is a common amphibole mineral that may occur in very similar rocks (both are common in granitoids) and may look alike. What is Muscovite The only easy way to distinguish the two is by their occurrence. Muscovite and biotite are phyllosilicate minerals. Tonalite pegmatite (white-gray on the right) and garnet amphibolite (on the left). 1. Its most important characteristic feature is its highly perfect basal cleavage. Carbonatite is igneous rock with highly unusual carbonate composition (white mineral is calcite). If present, biotite may be partially altered to other minerals. It is lightweight, reflective, refractive, flexible, and elastic. However, muscovite is much lighter in color than biotite, typically being colorless to white. The most characteristic property of these minerals is the perfect basal cleavage: They are black to dark-green, silicate minerals containing iron and magnesium. The micas, biotite and muscovite, both exhibit one direction of cleavage. Evje, Norway.
Metapelitic rocks that contain lots of biotite are various schists (biotite schist, biotite-chlorite schist, albite-biotite schist, garnet-mica schist). NOTEWORTHY LOCALITIES. 1. Moreover, its chemical formula can be given as K(Mg,Fe)3AlSi3O10(F,OH)2. 3. 5. Their hardness on the Mohs scale is only about 2.5-3 which is low for a silicate mineral (although within normal range for a sheet silicate). Larvik, Norway. That gives rise to the most characteristic feature of micas: perfect basal cleavage. muscovite. Biotite is in most cases not difficult to identify. Note how the elongated patches are oriented sub-parallel to each-other. It is usually phlogopite when biotite group mica is associated with carbonate minerals in igneous or metamorphic rocks. This rock (pure biotite-rock is known as glimmerite) formed similarly as part of pegmatite, but the source of fluids was mafic (gabbroic) magma which contained significantly more magnesium than felsic magma and favored the formation of phlogopite. Peraluminous two-mica granitoid. It is not as resistant in the weathering environment as muscovite and gets less frequent with extended transport. True False. Black mica and "white mica" (muscovite) often occur together within a rock and may even be found side-by-side. An Introduction to the Rock-Forming Minerals, 2nd Edition. It has a vitreous to pearly lustre. Trælen, Senja, Norway. The sample is from the type locality (Zinnwald) at the German/Czech border in The Ore Mountains. It is used as a filler and insulating material in the construction industry. So, the key difference between muscovite and biotite is that muscovite contains mainly potassium and aluminium, while biotite mainly contains potassium and magnesium. Senja, Norway. Width of sample 9 cm. Biotite finally disappears at the granulite facies conditions where hydrous minerals (which it is) are not stable. ";s:7:"keyword";s:21:"biotite and muscovite";s:5:"links";s:1432:"<a href="http://testapi.diaspora.coding.al/topics/beverly%2C-wv-zip-code-efd603">Beverly, Wv Zip Code</a>,
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