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Relevant bibliographies by topics / Muscoviti

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Journal articles

Academic literature on the topic 'Muscoviti'

Author: Grafiati

Published: 14 March 2023

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Journal articles on the topic "Muscoviti"

1

Monier, Gilles, and Jean-Louis Robert. "Muscovite solid solutions in the system K2O-MgO-FeO-Al2O3-SiO2-H2O: an experimental study at 2 kbar PH2O and comparison with natural Li-Free white micas." Mineralogical Magazine 50, no. 356 (1986): 257–66. http://dx.doi.org/10.1180/minmag.1986.050.356.08.

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AbstractThis paper presents the results of an experimental study of muscovite solid solutions in the system K2O-M2+O-Al2O3-SiO2-H2O-(HF), with M2+ = Mg2+ or Fe2+ in the temperature range 300-700°C under 2 kbar PH2O. Muscovite solid solutions can be described, in this system, as the result of two substitutions. One is the phengitic substitution (x), which preserves the pure dioctahedral character of the mica; the second is the biotitic substitution (y), which leads to trioctahedral micas and does not change the composition of the tetrahedral layer Si3Al. The general formula of muscovite in this

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2

Peruzzo, Luca, Raffaele Sassi, and F. P. Sassi. "Sulla vanabilità compositiva delle miche nell’amhito di uno stesso affioramento di metapeliti di basso grado: un esempio. 2: Le muscoviti e considerazioni conclusive." Rendiconti Lincei 3, no. 1 (1992): 43–55. http://dx.doi.org/10.1007/bf03002963.

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3

Dallmeyer, R. D., J. D. Keppie, and R. D. Nance. "40Ar/39Ar ages of detrital muscovite within Lower Cambrian and Carboniferous clastic sequences in northern Nova Scotia and southern New Brunswick: implications for provenance regions." Canadian Journal of Earth Sciences 34, no. 2 (1997): 156–68. http://dx.doi.org/10.1139/e17-013.

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Detrital muscovite from lowermost Cambrian sequences exposed in the Avalon Composite Terrane in Nova Scotia and New Brunswick record 40Ar/39Ar plateau ages of ca. 625–600 Ma. These are interpreted to date times of cooling in source areas. The regional distribution of coarse-grained detrital muscovite in Lower Cambrian rocks of Avalonian overstep sequences suggests a source region of dimensions considerably larger than any presently exposed in Appalachian segments of the Avalon Composite Terrane. Late Proterozoic tectonic reconstructions locate the Avalon Composite Terrane adjacent to northwest

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4

Treloar, Peter J. "Chromian muscovites and epidotes from Outokumpu, Finland." Mineralogical Magazine 51, no. 362 (1987): 593–99. http://dx.doi.org/10.1180/minmag.1987.051.362.14.

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AbstractThe Outokumpu region of Finland is notable for the large number of Cr-rich silicate and oxide phases associated with the massive sulphide deposits. In this paper analyses of Cr-rich phases in the epidote-clinozoisite and muscovite groups are presented. The muscovite-type phase shows a maximum 80% substitution of Cr for A1 on octahedral sites with a maximum 24.7 wt.% Cr2O3. Apparent complete solid solution between this extreme composition and the fuchsitic muscovites is indicated. The clinozoisite type phase has a maximum 15.4 wt.% Cr2O3, with a composition close to Ca2CrAl2Si3O12(OH).

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5

Pereira, Ronaldo Mello, Diana Rodrigues, Ciro Alexandre Ávila, and Reiner Neumann. "Stockscheider Quartzo-Moscovíticos e Pegmatíticos na Zona de Cúpula do Granitóide Ritápolis, Região de São João del Rei, Minas Gerais." Anuário do Instituto de Geociências 34, no. 2 (2011): 59–69. http://dx.doi.org/10.11137/2011_2_59-69.

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Clusters of essentially quartz-muscovitic rocks were found in four areas of the São João del Rei Pegmatite Province in close association with pegmatites positioned parallel to the contact between the Ritápolis granitoid and the metavolcanic - metasedimentary rocks of the Rio das Mortes greenstone belt. The suite of accessory minerals associated to the quartz-muscovite and pegmatite stockscheider (columbite-tantalite, cassiterite, gahnite, zircon, xenotime and monazite) are similar to those determined for the pegmatites of the province. The mineralogy of inclusions (Pb-tantalite, microlite, Pb-

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6

Halperin, Charles J. "“Scratch a Russian, Find a Turk”." Russian History 45, no. 4 (2018): 367–77. http://dx.doi.org/10.1163/18763316-04504004.

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In this first-rate monograph, Cornelia Soldat confirms earlier impressionistic assertions that the portrayal of Ivan iv as a tyrant and the Muscovites as barbarians in German-language pamphlets (Flugschriften) written as propaganda during the Livonian War (1558–1582), are simply projections onto the Muscovite discourse of the motifs of the anti-Ottoman discourse that originated in the fifteenth century after the fall of Constantinople in 1453. Therefore the pamphlets have no value whatsoever for the study of sixteenth- and seventeenth-century Muscovite history. These conclusions have wider sig

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7

Brown, Peter B. "Muscovite Arithmetic in Seventeenth-Century Russian Civilization: Is It Not Time to Discard the “Backwardness” Label?" Russian History 39, no. 4 (2012): 393–459. http://dx.doi.org/10.1163/48763316-03904001.

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Muscovite civilization utilized Byzantine-Greek alphanumerals for its mathematical symbols. Occasionally derided by historians for being retrograde in comparison to the Hindu-Arabic numerals sixteenth- and seventeenth-century Europe adopted, Muscovy’s alphanumerals were versatile and suitably contoured to perform a variety of computational tasks. Muscovite alphanumerals were an integral part of early Moderen Russia’s administrative culture, and played a prominent role in fostering the experiential knowledge underlying the educational achievements of the Imperial Period. Though they lacked the

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8

Ružička, Peter, Pavol Myšľan, and Sergii Kurylo. "Minerálne zloženie metapelitovej a metapyroklastickej zložky kryštalických vápencov z lokalít Lubeník a Ochtiná (Slovenská republika)." Bulletin Mineralogie Petrologie 28, no. 2 (2020): 281–89. http://dx.doi.org/10.46861/bmp.28.281.

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Crystalline limestones from the localities Lubeník and Ochtiná (Slovak Republic) have been formed by recrystallization of limestones enriched by basaltic tuffogenic material and a minor pelitic component. The regional metamorphism and tectonic activity associated with Alpine orogennesis resulted in origin of various color and textural varieties of crystalline limestones. The recrystallized tuffogene-pelitic material was transformed into the laminar arrangement in crystalline limestones. The original clay-like pelitic component has probably been entirely recrystallized into muscovite. Higher co

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9

Selin, Adrian Aleksandrovich. "«Expelled from Livonia»: Towards the issue of the arrangement of landowners of «Old» and «New German towns» after the Plyussa Treaty 1583." Studia Slavica et Balcanica Petropolitana, no. 2 (28) (2020): 24–35. http://dx.doi.org/10.21638/spbu19.2020.202.

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History of Muscovite estate shaping in “German towns” in 1550s–1580s is closely connected with Novgorod, Pskov, Rzheva Pustaya as servicemen communities. These servicemen were the source for new landowners in the lands taken by Muscovites to the West from Narova river. Only Rzheva Pustaya was more or less studied already. The paper is an attempt to generalize the data on number and personal content of “German towns” landowners (mostly on sources of 1582) and to study the issue of the significance of the experience of making estates in Livonian lands for the day-to-day culture of Muscovite serv

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10

Halperin, Charles J. "Ivan IV and the Tatars." Golden Horde Review 9, no. 1 (2021): 188–200. http://dx.doi.org/10.22378/2313-6197.2021-9-1.188-200.

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Research objectives: To provide a comprehensive overview of Muscovite interaction with Tatars during Ivan IV’s reign, both with each successor state of the Jochid ulus and with Tatars who moved to Muscovy and entered Ivan IV’s service. Research materials: This study is based upon Russian sources from the reign of Ivan IV concerning the Tatars, including narratives such as chronicles and documentary evidence such as diplomatic reports. Results and novelty of the research: Muscovite policy toward the Tatars did not derive from a single dominating motive, neither hostility, such as religious anim

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