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Upper Chegem Caldera

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Journal Article
Published: 16 September 2015
The Canadian Mineralogist (2015) 53 (2): 325–344.
... (SiO 4 ) 3 (ОН) 2 [ Pbnm , a 5.0696(1), b 11.3955(1), c 23.5571(3) Å, V 1360.91(4) Å 3 , Z = 4], was found in an edgrewite-bearing zone of endoskarn at the contact of a large altered calciferous xenolith within ignimbrites of the Upper Chegem Caldera, Northern Caucasus, Kabardino-Balkaria, Russia...
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Journal Article
Published: 01 August 2013
Mineralogical Magazine (2013) 77 (6): 2857–2866.
...I. O. Galuskina; E. V. Galuskin; K. Prusik; V. M. Gazeev; N. N. Pertsev; P. Dzierżanowski Abstract Irinarassite, Ca 3 Sn 2 SiAl 2 O 12 , a new mineral species of the garnet supergroup was discovered in metasomatically altered carbonate-silicate xenoliths in ignimbrites of the Upper Chegem Caldera...
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Journal Article
Published: 01 May 2013
European Journal of Mineralogy (2013) 25 (2): 231–239.
..., was discovered in a kumtyubeite zone in close proximity to the contact with unaltered ignimbrite in a skarn xenolith from the Upper Chegem Caldera, Northern Caucasus, Russia. The empirical formula of the holotype dzhuluite is (Ca 2.954 Fe 2+ 0.043 Mg 0.003 ) ∑3.000 (Sn 0.850 Sb 5+ 0.764 Zr 0.121 U 6+ 0.127 Ti 4...
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Journal Article
Published: 01 November 2012
American Mineralogist (2012) 97 (11-12): 1998–2006.
... skarn within the Upper Chegem caldera, Northern Caucasus, Kabardino-Balkaria, Russia. The xenolith containing the two new minerals crops out on the slope of the small ridge joining Lakargi and Vorlan peaks at 3240 m above the sea level and 7 km from the Balkarian village Eltyubyu. Other Ca humite group...
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Journal Article
Published: 01 April 2012
American Mineralogist (2012) 97 (4): 503–512.
... with dellaite Ca 6 (Si 2 O 7 )(SiO 4 )(OH) 2 around galuskinite Ca 7 (SiO 4 ) 3 CO 3 veins cutting calcio-olivine skarns in the Birkhin gabbro massif. In addition, skeletal pavlovskyite occurs in cuspidine zones of altered carbonate xenoliths in the ignimbrites of the Upper Chegem caldera (North Caucasus...
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Journal Article
Published: 01 October 2011
European Journal of Mineralogy (2011) 23 (5): 837–844.
... of the Upper Chegem volcanic caldera. The mineral is named after Vladimir Leonidovich Rusinov (1935–2007), a Russian petrologist and expert in the field of thermodynamics of non-equilibrium mineral systems. A synthetic analogue of rusinovite is also known. The new mineral has an OD structure of which only...
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Journal Article
Published: 01 October 2011
Mineralogical Magazine (2011) 75 (5): 2563–2572.
...E. V. Galuskin; I. O. Galuskina; V. M. Gazeev; P. Dzierżanowski; K. Prusik; N. N. Pertsev; A. E. Zadov; R. Bailau; A. G. Gurbanov Abstract Megawite is a perovskite-group mineral with an ideal formula CaSnO 3 that was discovered in altered silicate-carbonate xenoliths in the Upper Chegem caldera...
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Journal Article
Published: 01 January 2011
American Mineralogist (2011) 96 (1): 188–196.
... = 4–5, VHN 10 = 360 kg/mm 2 , was found near the top of Mt. Vorlan in a calcareous skarn xenolith in ignimbrite of the Upper Chegem caldera in the Northern Caucasus, Kabardino-Balkaria, Russia. Vorlanite occurs as aggregates of black platy crystals up to 0.3 mm long with external symmetry 3̅ m...
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Journal Article
Published: 01 August 2010
American Mineralogist (2010) 95 (8-9): 1172–1181.
... , a new uranian garnet ( Ia <ovl>3</ovl> d , a ≈ 12.55 Å, V ≈ 1977 Å 3 , Z = 8), within the complex solid solution elbrusite-kimzeyite-toturite Ca 3 (U,Zr,Sn,Ti,Sb,Sc,Nb...) 2 (Fe,Al,Si,Ti) 3 O 12 was discovered in spurrite zones in skarn xenoliths of the Upper Chegem caldera. The empirical...
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Fig. 1.
Published: 16 September 2015
F ig . 1. Geological map of the Upper Chegem Caldera (after Gazeev et al . 2006 and Galuskin et al . 2009 , simplified). The inset map shows the location of Kabardino-Balkaria. Legend: (1–5) Formations of different ages of the volcanic basement. 1,2 Structural zone of the Greater Caucasus
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Fig. 2.
Published: 16 September 2015
F ig . 2. (A) General view of the northwest part of the Upper Chegem Caldera; numbers indicate xenoliths and their positions. Xenoliths are distinguished on the ignimbrite background by a white color. (B) xenolith no. 1 in the foreground, type locality of fluorchegemite. The distance between
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Compositions of U-rich garnets from the Upper Chegem caldera, Northern Caucasus, Russia (Galuskina et al. 2010a; Utsunomiya et al. 2002). The red lines mark the boundaries between elbrusite, kerimasite and an unnamed species based on the relative proportions of the kerimasite end-member, new elbrusite end-member and the unnamed {Ca3}[U26+](R32+)O12 end-member. Yellow circle indicates the Sn-dominant analog of elbrusite, which was included in the least-squares fit.
Published: 01 April 2013
Figure 4 Compositions of U-rich garnets from the Upper Chegem caldera, Northern Caucasus, Russia ( Galuskina et al. 2010a ; Utsunomiya et al. 2002 ). The red lines mark the boundaries between elbrusite, kerimasite and an unnamed species based on the relative proportions of the kerimasite end
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Raman spectra of trabzonite from the Upper Chegem caldera, Northern Caucasus. Spectra are as follows: (1) a pseudomorph (Fig. 2b); (2) a spherulite (Fig. 2a); (3) an aggregate with killalaite (Fig. 2c).
Published: 01 June 2012
F ig . 3. Raman spectra of trabzonite from the Upper Chegem caldera, Northern Caucasus. Spectra are as follows: (1) a pseudomorph ( Fig. 2 b ); (2) a spherulite ( Fig. 2 a ); (3) an aggregate with killalaite ( Fig. 2 c ).
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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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Megawite and lakargiite in skarns of the Upper Chegem caldera: (a–c) spurrite skarns from xenolith no. 1; (a) megawite crystals are found only inside spurrite grains (magnified fragment is shown in inset), whereas lakargiite is widespread in both spurrite and wadalite-hydrocalumite-calcite aggregate; (b) spurrite crystal etched in 10% HCl with megawite and wadalite inclusions (a magnified image of a megawite crystal is shown in inset); (c) megawite and lakargiite in a fractured spurrite crystal (see description in the text); (d) pseudo-cubic crystals of high-Sn lakargiite overgrowing a porous aggregate of lakargiite and srebrodolskite from the chegemite zone of xenolith no. 7; (e) crystals of high-Sn lakargiite with external zones of megawite growing over a fine-grained lakargiite-wadalite-hibschite aggregate, burtite CaSn(OH)6 also occurs in this association; (f) megawite and garnet forming later zones in complex pseudomorphs after zircon, from the larnite-cuspidine zone of xenolith no. 3 (a zoned crystal comprising a lakargiite core and a megawite rim is shown inset). Arabic numerals show the sites of the EMPA analyses. Abbreviations are: Meg, megawite; Afw, afwillite; Brc, brucite; Brt, burtite; Cal, calcite; Chg, chegemite; Etr, ettringite; Hgr, hydrogrossular; Hil, hillebrandite; Hcl, hydrocalumite; Lak, lakargiite; Lar, larnite; Rnd, rondorfite; Sch, schorlomite; Spu, spurrite; Srb, srebrodolskite; Tot, toturite; Wad, wadalite.
Published: 01 October 2011
F ig . 1. Megawite and lakargiite in skarns of the Upper Chegem caldera: ( a – c ) spurrite skarns from xenolith no. 1; ( a ) megawite crystals are found only inside spurrite grains (magnified fragment is shown in inset), whereas lakargiite is widespread in both spurrite and wadalite
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Raman spectra of killalaite: (1) on a cross-section approximately perpendicular to z from the Upper Chegem caldera, Northern Caucasus (Fig. 2d); (2) on a cross-section approximately parallel to z from the Upper Chegem caldera, Northern Caucasus (Fig. 2d); (3) intergrowths with trabzonite from the Upper Chegem caldera, Northern Caucasus (Fig. 2c); (4) on a specimen from Ikizdere, Turkey (Fig. 1).
Published: 01 June 2012
F ig . 4. Raman spectra of killalaite: (1) on a cross-section approximately perpendicular to z from the Upper Chegem caldera, Northern Caucasus ( Fig. 2 d ); (2) on a cross-section approximately parallel to z from the Upper Chegem caldera, Northern Caucasus ( Fig. 2 d ); (3) intergrowths
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Raman spectra of killalaite in the OH region: (1) on a cross-section approximately perpendicular to z from the Upper Chegem caldera, Northern Caucasus (Fig. 2d); (2) on a cross-section approximately parallel to z from the Upper Chegem caldera, Northern Caucasus (Fig. 2d); (3) intergrowths with trabzonite from the Upper Chegem caldera, Northern Caucasus (Fig. 2c); (4) specimen from Ikizdere, Turkey (Fig. 1).
Published: 01 June 2012
F ig . 5. Raman spectra of killalaite in the OH region: (1) on a cross-section approximately perpendicular to z from the Upper Chegem caldera, Northern Caucasus ( Fig. 2 d ); (2) on a cross-section approximately parallel to z from the Upper Chegem caldera, Northern Caucasus ( Fig. 2 d ); (3
Journal Article
Published: 01 January 2015
European Journal of Mineralogy (2015) 27 (1): 113–122.
...)Å, V =1740.34(3)Å 3 ), was discovered as an accessory mineral in Ca-humite zones of calcareous skarn xenoliths in ignimbrites of the Upper Chegem Caldera, Northern Caucasus, Kabardino-Balkaria, Russia. Rounded grains and crystals with tris-tetrahedral form of chlorkyuygenite up to 50μm and aggregates...
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Journal Article
Published: 01 November 2013
American Mineralogist (2013) 98 (11-12): 1938–1942.
... Upper Chegem caldera, Northern Caucasus. Heating above 750 °C of dark-gray vorlanite from the Jabel Harmun, as well as dark-red vorlanite from Caucasus, led to formation of yellow trigonal uranate CaUO 4 . The unusual color of vorlanite from Jabel Harmun is assumed to be related to small impurities...
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Journal Article
Published: 01 May 2013
European Journal of Mineralogy (2013) 25 (2): 221–229.
... Al 10 Si 4 O 32 Cl 6 , was discovered in altered silicate-carbonate xenoliths in the diatreme facies of ignimbrites in the Upper Chegem caldera, Kabardino-Balkaria, Northern Caucasus, Russia. Eltyubyuite forms light-brown or yellow crystals with tetrahedral habit up to 10 μm across in rondorfite...
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