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rusinovite

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Journal Article
Published: 01 October 2011
European Journal of Mineralogy (2011) 23 (5): 837–844.
...Evgeny V. Galuskin; Irina O. Galuskina; Biljana Lazic; Thomas Armbruster; Aleksandr E. Zadov; Tomasz Krzykawski; Kamila Banasik; Viktor M. Gazeev; Nikolai N. Pertsev Abstract Rusinovite, Ca 10 (Si 2 O 7 ) 3 Cl 2 , was discovered in an altered carbonate-silicate xenolith enclosed in ignimbrites...
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(a) – fragment of rankinite partially replaced by rusinovite and trabzonite. (b) – fragment of pavlovskyite pseudomorph with cuspidine rims after an early rankinite pseudomorph (after wollastonite?) in a rusinovite zone. (c) – rondorfite relics in the rusinovite zone. (d) – solitary rusinovite crystals in pseudomorph of wollastonite after quartz (central fragment of oval pseudomorph). Rusinovite displays a clear zonal structure emphasized by dispersed inclusions of wollastonite in the grey central sectors). BSE images, Rus – rusinovite, Wol – wollastonite, Wad – wadalite, Cus – cuspidine, Hgr – hydrogrossular, Rnd – rondorfite, Pav- pavlovskyite, Trb – trabzonite, Ran – rankinite, Hil –hillebrandite, Hds – unidentified hydrosilicates.
Published: 01 October 2011
Fig. 2. (a) – fragment of rankinite partially replaced by rusinovite and trabzonite. (b) – fragment of pavlovskyite pseudomorph with cuspidine rims after an early rankinite pseudomorph (after wollastonite?) in a rusinovite zone. (c) – rondorfite relics in the rusinovite zone. (d) – solitary
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Rusinovite spherulite in endoskarn: A, B – transmitted light, parallel nicols (a) and crossed nicols (b). (c) – BSE image, the frames indicate magnified fragments shown in Fig. 1d and e. (d) – replacement of rusinovite by trabzonite. Trabzonite has wadalite inclusions, which are altered to hydrogrossular. (e) –Rusinovite and wadalite aggregates on the border to a rusinovite spherulite, which was not altered by hydration. Rus – rusinovite, Wad – wadalite, Hgr – hydrogrossular (hibschite-katoite series), Trb – trabzonite, Jen – jennite.
Published: 01 October 2011
Fig. 1. Rusinovite spherulite in endoskarn: A, B – transmitted light, parallel nicols (a) and crossed nicols (b). (c) – BSE image, the frames indicate magnified fragments shown in Fig. 1d and e . (d) – replacement of rusinovite by trabzonite. Trabzonite has wadalite inclusions, which are altered
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A: Contact of xenolith with volcanic rock (polished block): 1–volcanic rock, 2–altered xenolith, 3–rusinovite–cuspidine vein. B: Backscattered electron image showing a fragment of rusinovite–cuspidine vein with eltyubyuite. (online version in colour) Abbreviations: Rus = rusinovite, Cus = cuspidine, Hcl = hydrocalumite, Wol = wollastonite, Elt = eltyubyuite, Rnd = rondorfite.
Published: 01 January 2015
Fig. 1 A: Contact of xenolith with volcanic rock (polished block): 1–volcanic rock, 2–altered xenolith, 3–rusinovite–cuspidine vein. B: Backscattered electron image showing a fragment of rusinovite–cuspidine vein with eltyubyuite. (online version in colour) Abbreviations: Rus = rusinovite, Cus
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Upper Chegem caldera: (a and b) BSE images of aggregates of pavlovskyite in cuspidine skarn. (c) BSE image of pavlovskyite-hillebrandite aggregate (after rankinite) in a rusinovite zone of skarn. (d–f) Quartz grain on the boundary between ignimbrite and skarn, the grain is partially replaced by pavlovskyite, rankinite, wollastonite, and hillebrandite aggregates. (d) BSE, (e) plane-polarized light, (f) crossed polarizers. Pav = pavlovskyite, Rus = rusinovite, Ran = rankinite, Wol = wollastonite, Cus = cuspidine, Wad = wadalite, Hil = hillebrandite, Q = quartz, Ap = fluorapatite, Hgr = hydrogrossular.
Published: 01 April 2012
Figure 2 Upper Chegem caldera: ( a and b ) BSE images of aggregates of pavlovskyite in cuspidine skarn. ( c ) BSE image of pavlovskyite-hillebrandite aggregate (after rankinite) in a rusinovite zone of skarn. ( d – f ) Quartz grain on the boundary between ignimbrite and skarn, the grain
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Raman spectra of rusinovite (1) and rankinite (2) from Lakargi skarns.
Published: 01 October 2011
Fig. 3. Raman spectra of rusinovite (1) and rankinite (2) from Lakargi skarns.
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Crystal structure of rusinovite projected along a; two types of Si2O7 disilicate units are distinguished; Si1 and Si2 tetrahedra are red and yellow, respectively. Oxygen sites are represented as small light blue spheres, Ca sites are dark blue, Cl is green; unit cell is shown by solid black outlines.
Published: 01 October 2011
Fig. 4. Crystal structure of rusinovite projected along a ; two types of Si 2 O 7 disilicate units are distinguished; Si1 and Si2 tetrahedra are red and yellow, respectively. Oxygen sites are represented as small light blue spheres, Ca sites are dark blue, Cl is green; unit cell is shown
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Average structure of rusinovite projected along a as in Fig. 4 but, in addition, Ca3O8 cubes are shown to emphasize undulating layers parallel to (010). Si2O7 dimers extend parallel to a.
Published: 01 October 2011
Fig. 7. Average structure of rusinovite projected along a as in Fig. 4 but, in addition, Ca3O 8 cubes are shown to emphasize undulating layers parallel to (010). Si 2 O 7 dimers extend parallel to a .
Journal Article
Published: 01 November 2015
Russ. Geol. Geophys. (2015) 56 (11): 1603–1621.
...” CaFe 4 O 7 , and “dorrite phase” Ca 2 ( Fe 5 3+ Mn 0.5 3+ Mg 0.5 )(Si 0.5 Fe 5.5 3+ )O 20 ) and, rarely, as individuals in grained aggregates of fluorellestadite–cuspidine (± larnite ± rusinovite Ca 10 (Si 2 O 7 ) 3 Cl 2 ). Assemblages of zoned chlormayenite–wadalite crystals are found in grained...
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Journal Article
Published: 01 January 2015
European Journal of Mineralogy (2015) 27 (1): 137–143.
...Fig. 1 A: Contact of xenolith with volcanic rock (polished block): 1–volcanic rock, 2–altered xenolith, 3–rusinovite–cuspidine vein. B: Backscattered electron image showing a fragment of rusinovite–cuspidine vein with eltyubyuite. (online version in colour) Abbreviations: Rus = rusinovite, Cus...
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Journal Article
Published: 01 April 2014
American Mineralogist (2014) 99 (4): 870–875.
..., Washington D.C., U.S.A. (NMNH 174253). G.D.G. and F.C. © 2014 Mineralogical Society of America 2014 This New Mineral Names has entries for nine new minerals, including clinometaborite, hughesite, kirchhoffite, mendeleevite-(Ce), parasterryite (along with new data for sterryite), rusinovite...
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Fig. 8.
Published: 16 September 2015
. Figures 8C–G were produced with back scattered electrons (BSE). (D) Wollastonite micro-zone decorating the contact with quartz. (E) Larnite lens-like aggregate containing rankinite relics (grey). (F) Hydroxyledgrewite lens with larnite relics. (G) Rare type of lens-like aggregates of rusinovite (grey
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Back-scattered electron image of a skarn sample from the Upper Chegem caldera, Northern Caucasus. (a) Trabzonite spherulites in fractures of the endoskarn zone (from xenolith no. 5). (b) Incomplete pseudomorphic replacement of trabzonite after rankinite–pavlovskyite intergrowths (from xenolith no. 3). (c) Trabzonite surrounded by aggregates of killalaite (from xenolith no. 3). (d) Killalaite and hydroxylellestadite crystals in altered larnite skarn (from xenolith no. 7). Mineral abbreviations are Cus, cuspidine; Ell, hydroxylellestadite; Etr, ettringite; Hil, hillebrandite; Hgr, hydrogrossular; Kil, killalaite; Pav, pavlovskyite; Ran, rankinite; Rus, rusinovite; Trb, trabzonite; Wad, wadalite.
Published: 01 June 2012
; Hgr, hydrogrossular; Kil, killalaite; Pav, pavlovskyite; Ran, rankinite; Rus, rusinovite; Trb, trabzonite; Wad, wadalite.
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BSE images showing the proportions of opaque and silicate minerals in metacabonate rock from spoil heap of the Baturinskaya-Vostochnaya-1-2 mine, Emanzhelinsk, and selected regions of rock. Ore, Opaque aggregates; La, larnite; Cus, cuspidine; Ell, fluorellestadite; Ap, fluorapatite; Rnd, rondorfite; Mg-Cus, “Mg-cuspidine”; F-Rnd, F-analog of rondorfite; Grf, “grandiferrite” CaFe4O7; F-Elt, F-analog of eltyubyuite; Sym, cavernous aggregate formed of Ca-ferrite (“grandiferrite”) and/or “dorrite phase” and cuspidine (± anhydrite ± fluorellestadite); Hem, hematite; Mgf, magnesioferrite; Rus, rusinovite. Sample E-4-8, zoned yellow-colored aggregate.
Published: 01 November 2015
, rusinovite. Sample E-4-8, zoned yellow-colored aggregate.
Journal Article
Published: 16 September 2015
The Canadian Mineralogist (2015) 53 (2): 325–344.
... . Figures 8C–G were produced with back scattered electrons (BSE). (D) Wollastonite micro-zone decorating the contact with quartz. (E) Larnite lens-like aggregate containing rankinite relics (grey). (F) Hydroxyledgrewite lens with larnite relics. (G) Rare type of lens-like aggregates of rusinovite (grey...
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Journal Article
Published: 01 April 2012
American Mineralogist (2012) 97 (4): 503–512.
...Figure 2 Upper Chegem caldera: ( a and b ) BSE images of aggregates of pavlovskyite in cuspidine skarn. ( c ) BSE image of pavlovskyite-hillebrandite aggregate (after rankinite) in a rusinovite zone of skarn. ( d – f ) Quartz grain on the boundary between ignimbrite and skarn, the grain...
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Journal Article
Published: 01 June 2012
Mineralogical Magazine (2012) 76 (3): 455–472.
...; Hgr, hydrogrossular; Kil, killalaite; Pav, pavlovskyite; Ran, rankinite; Rus, rusinovite; Trb, trabzonite; Wad, wadalite. ...
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Journal Article
Published: 01 April 2011
Mineralogical Magazine (2011) 75 (2): 289–294.
...., Armbruster, T., Zadov, A.E., Krzykawski, T., Banasik, K., Gazeev, V.M. and Pertsev, N.N. (2011) Rusinovite, IMA 2010-072. CNMNC Newsletter No. 8, April 2011, page 292; Mineralogical Magazine , 75 , 289–294. IMA No. 2010-059 Ernstburkeite Mg(CH 3 SO 3 ) 2 ·12H 2 O In an ice core from...
Journal Article
Published: 01 February 2013
American Mineralogist (2013) 98 (2-3): 493–500.
... material with Ca/Si = 1.72. The Ca/Si ratio should be 2 for rustumite. Their analysis is more consistent with the composition of the new mineral rusinovite Ca 10 (Si 2 O 7 ) 3 Cl 2 ( Galuskin et al. 2011 ). Furthermore, formation of rustumite under pyrometamorphic conditions is rather doubtful due...
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Journal Article
Published: 01 October 2011
Mineralogical Magazine (2011) 75 (5): 2563–2572.
..., page 290 ; Mineralogical Magazine , 75 , 289 – 294 . Galuskin , E.V. , Galuskina , I.O. , Lazic , B. , Armbruster , T. , Zadov , A.E. , Krzykawski , T. , Banasik , K. , Gazeev , V.M. and Pertsev , N.N. ( 2011 c) Rusinovite, IMA 2010-072. CNMNC Newsletter...
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