muscovite in English
The intervening host-rock layers are between 2 and 5 cm thick, being composed of biotite, sillimanite, garnet, muscovite , quartz and plagioclase.
A native Muscovite adds: ‘It's difficult to say why it's like this in Russia - are things this bad because the men drink or do they drink because things are this bad?’
In his world - the world of a Muscovite professional - this meant that the city's middle class has finally broken through the cocoon of insecurity; it started earning and spending money.
Use "muscovite" in a sentence
1. 5 out of 5 stars (101) $ 37.99 FREE shipping Add to Favorites Beryl Muscovite Ring / Beryl Muscovite Silver Ring / Natural Beryl Muscovite Handmade Jewelry / 925 Sterling Silver Ring / Silver
2. Muscovite is a thin type of rock formation.
3. Unlisted Muscovite Hayden royalizes carbonation Barbarizes overexcited invectively.
4. This is attributed to the presence of Rb-poor muscovite and Sr-rich barite.
5. For the health-conscious Muscovite, another Soviet legacy is potentially more nerve-wracking still.
6. 17 Grams Very Beautiful Combination of Columbite Apatite and Muscovite Crystal From Skardu Pakistan ssminerals
7. Silicates (muscovite, albite, chlorite, labradorite, actinolite, and orthoclase) occur in high concentrations.
8. Moskvitin reported his discoveries to Prince Shcherbatov, the Muscovite voivode in Tomsk.
9. All rocks contain quartz, alkali feldspar, plagioclase, muscovite, and biotite (with the exception of some leucocratic dykes).
10. Muscovite is in demand for the manufacture of fireproofing and insulating materials and to some extent as a lubricant.
11. The Batholiths comprise biotite, hornblende–biotite, and biotite–muscovite granite and granodiorite (Kwon et al., 1995a; Sagong et al., 1997).
12. Mordvinov's independent-mindedness and Anglophile way of life made him a darling of the Muscovite society.
13. Hydrothermal veins containing quartz, muscovite, amblygonite-montebrasite, apatite, fluorite, and/or cassiterite appear spatially related to the tourmalinites.
14. Muscovite is the main indicator mineral for alkalic alteration and occurs in veins that contain anorthoclase or quartz.
15. With increasing metamorphic grade the retrograde process of saussuritization is initiated. The reactants are Fe (III) Al2-epidote, muscovite, quartz, hematite, and albite/ oligoclase.
16. 9 The nodule minerals consist of quartz, plagioclase, amphibole, K ? feldspar , goethite, lepidocrocite, δ MnO ? 2 , illite, and muscovite etc.
17. Tourmalinites composed of tourmaline, quartz, plagioclase, ± almandine-rich garnet, ± muscovite, ± biotite, and minor ilmenite, rutile, graphite,- ± pyrite and, rarely, scheelite are of pre- to synmetamorphic origin.
18. Coexisting minerals with beryl are quartz, plagioclase, K-feldspar, biotite, muscovite, margarite, chlorite, talc, amphibole, epidote, garnet, phenakite, calcite, fluorite (+accessory phases).
19. The 579.8 ± 2.2 Ma (40Ar-39Ar, muscovite) Georgeville Pluton in mainland Nova Scotia is an epizonal body consisting of alkali feldspar granite and related pegmatite.
20. Metapelites with the assemblage garnet-staurolite-kyanite-sillimanite±andalusite-biotite-muscovite-plagioclase were used to reconstruct pressure and temperature conditions with exchange thermometry, net transfer equilibria and multi-equilibrium methods.
21. Cale-silicate mica schists of higher-medium grade carry mutually stable calcic scapolite, andesine and zoisite, associated with calcite, quartz, local epidote, biotite, muscovite, and garnet.
22. Late-hercynian granodiorites in the eastern Serre are calc-alkaline and peraluminous in composition; actinolitic-hornblende typically occurs in the mafic types, whereas muscovite occurs in the felsic ones.
23. Temperature estimates from fluid-muscovite-quartz-feldspar equilibrium and oxygen isotope thermometry of coexisting adularia and quartz are combined with the fluid inclusion isochores to derive depositional pressures.
24. The inclusions are usually Muscovite mica, but may also be Hematite or Goethite.Though the color of Aventurine is most often associated with green, it can also be other colors such as gray, orange, and brown.
25. Epidote–amphibolite facies include the critical assemblage calcic pyroxene + calcic amphibole (magnesiohornblende and pargasite) + muscovite + garnet + plagioclase + epidote ± quartz, whereas greenschist facies is defined by the assemblage actinolite + albitic plagioclase + epidote + chlorite.
26. Biotite (4–7 vol.-%) forms the 2M polymorphe, as well as muscovite (6,5–7,5 vol.-%) which may develop by reaction of andalusite with the melt or from alkalifeldspar by reaction with the fluid phase.
27. The late granite dike suite, comprising late-stage, muscovite- and biotite-bearing quartz – alkali feldspar pegmatite and finer grained granitic lithologies, represents the last magmatic event in the Northern complex emplaced after collision.
28. Believers, Christians with a religious faith in the divine Christ; Believers (), a term in the Quran for MuslimsBelievers Church, a Pentecostalist church; Russian Old Believers, a sect who separated from the Muscovite Orthodox Church as a protest against church reforms
29. Authigenous quartz, muscovite and orthoclase were singled out from Triassic carbonate rocks that had been subjected to alteration in the surrounding fault breccia of Mangishlac (MLJRAVYOV, The origin of each of these minerals was 1964)
30. The sediments from the Moresby Canyon, the Coral Sea Abyssal Plain, and the northeastern slope of the Queensland Plateau have received their terrigenous components, mainly quartz, feldspar, chlorite and muscovite-illite from mainland New Guinea.
31. Glittery inclusions are typically composed of muscovite mica, which usually results in medium to dark green Aventurine stones with a silvery green or blue sheen.The metallic inclusions give Aventurine quartz a unique sparkling iridescent effect, known as 'aventurescence'.
32. ‘A plagioclase feldspar, Albite probably, occurs as parallel growths of transparent colorless to yellowish crystals.’ More example sentences ‘They collected several pegmatite pockets in which topaz was associated with both clear and smoky quartz, microcline, Albite, muscovite, fluorite, and cassiterite.’
33. The mineral assemblages are dominated by muscovite (25–45%), chlorite (15–25%), quartz (18–30%) and albite (2–6%) while hematite, dolomite, pyrite, apatite, ore, zircon, rutile and amorphous carbon are accessory, but in some rocks hematite (11%), dolomite (42%) and talc (40%) are also dominant.
34. This U – Pb age provides a new geochronologic "pin" in the evolution of the Yukon – Tanana terrane prior to its Mesozoic accretion to the North American continental margin and, combined with recent 40Ar/39Ar muscovite data, indicates that high-pressure metamorphism at this time was a relatively short-lived event.
35. Two grades of metamorphism, both subfacies of the greenschist facies of regional metamorphism, were mapped on the Araya Peninsula: 1. the quartzalbite-epidote-almandine subfacies, consisting mainly of a sequence of garnet and kyanite quartz-mica schists, interlayered with quartzites; and 2. the quartzalbite-muscovite-chlorite subfacies, which consists of chloritic phyllites, quartzmica schists and phyllites, metaconglomerates, calcareous quartz-mica schists, limestones and marbles, and calcareous epidote schists of volcanic origin.
36. Type I is represented by barren pegmatites with graphic textures; type II comprises transitional varieties with Li-Fe-Mn phosphates, Be (chrysoberyl) and scarce Nb-Ta and U oxide minerals; type III consists of pegmatites with significant zones of replacement containing Li-Fe-Mn phosphates, beryl and more abundant Nb-Ta oxide minerals; and type IV, muscovite-quartz-albite pegmatites are highly mineralized with Be, Nb-Ta and HREE.
37. Lepidolite and lithian muscovite occur in high-pressure spodumene, low-pressure petalite, phosphorus-enriched amblygonite and fluorine-rich lepidolite subtypes of orogenic affiliated complex type granitic pegmatites and rarely in anorogenic affiliated amazonite-bearing Trace element data determined by X-ray fluorescence for lepidolite of various pegmatite subtypes, morphology (“book”, “scaly”, “fine-grained”), position within the pegmatite (primary zones, replacement units, pockets), mineral assemblages and tectonic affinity (orogenic vs anorogenic) show extreme fractionation of Rb and Cs; modest levels of T1, Ga, Nb, Ta, Sn and Zn; and typically low abundances of Ba, Sr, Ni, Pb, Y, V, W and Zr.