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![First thumbnail for: Relation between cathodoluminescence and trace-ele...]()
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![First thumbnail for: Rb–Sr isotope system and Rb–Sr partitioning in the...]()
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![Sr–Rb ratio in the rocks of the Ary-Bulak massif. The element contents (Table 1) were determined by double isotopic dilution; in the other cases, by ICP analysis. 1, porphyritic ongonites; 2, porphyritic rocks with Ca–F glass; 3, aphyric rocks.]()
![Isochron Rb–Sr diagrams for the rocks of the Ary-Bulak massif. See description in the text.]()
![Ratios between the Sr isotope contents calculated for the rocks of the Ary-Bulak massif. See description in the text.]()
![Dependence of the measured 87Sr/86Sr ratio on the Sr content (a) and 1/Sr (b) of the rocks of the Ary-Bulak massif.]()
![Dependence of the initial Sr isotope ratio on the Sr content of the rocks of the Ary-Bulak massif. 1, 2, rocks of the massif; 3, 4, 87Sr/86Sr in the limestones of the Ust’-Borzya Formation (1, 4, authors’ data; 2, 3, after (Kostit-syn et al., 2004)).]()
![Normalized [20] REE patterns of granites of the Khangilai intrusion. Granites: 1 — MIP biotite granites, 2 — muscovite granites of exocontact dikes of the Spokoiny dome, 3 — muscovite granites of the Khangilai massif, 4 — granite-porphyries of the Ubzhigoi series, 5 — intensely greisenized muscovite granites of the Spokoiny dome, 6 — amazonite Li-F-granites of the Orlovka dome, 7 — ongonites of the Ary-Bulak massif (Sherlovaya Gora area). The curve numbers correspond to the run numbers in Table 2.]()
![Calcium fluoride phase (partly crystalline glass) in the Ca- and F-enriched rocks of the Ary-Bulak massif. a, Large segregations of the calcium fluoride phase (black areas) in Ca- and F-rich porphyritic rock (sample ARB131), viewed under ×-polars; b, groundmass (sample ARB148); c, area of an opened (unheated) melt inclusion from a quartz phenocryst (sample ARB24); d, opened (unheated) melt inclusion with Ca–F glass (sample ARB24); e, phenocrysts of Ca–F glass after melt inclusion heating to 900–950 °C (sample ARB23); b–d, fluorite crystals and segregations of dickite or kaolinite in Ca–F glass; b–e, back-scattered electron (BSE) images. Ca–F, calcium fluoride phase (glass); Gl, silicate glass; Fl, fluorite; Ab, albite; Sa, sanidine; Qtz, quartz; Mc, mica; Dc, dickite or kaolinite; g, remnants of the gas (shrinkage) bubble.]()
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![First thumbnail for: Ongonite–elvan magmas of the Kalguty ore-magmatic ...]()
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![A structural scheme of the East-Transbaikalian Cover-Folded Arch. Complexes: 1 – metamorphic (Lower Archean undivided complex and Borshchovochny Group of Lower Proterozoic age) and granite (Dyrbylkei Complex of Lower Proterozoic age) – AR1 + PR1; 2 – clay-silica-basalt (Kulinda Formation), sand-schistose (Onon and Urulyungui Formations), schist-sand-carbonate (Nortui Formation) – R1+2; 3 – granite (Urulyungui Complex, Late Riphean and polychronous granitoids) – R3–J; 4 – terrigenous-carbonate (Tsagan-Olo and Bystraya Formations) – V+Є1; 5 – volcanogenic-siliceous-sand-schistose (Chindat and Ust’-Borzya Formations) – D1–2; 6 – volcanogenic-siliceous-schistose-sandy (Urtui Formation) – C1; 7 – terrigenous (Borzya Formation) – P2; 8 – granite (Unda and Ingamakit Complexes) – Pz3; 9 – terrigenous (Mogoitui Group, Ikagin, Akatui, Bazanovo, and Onon-Borzya Formations) – T3+J1; 10 – sand-conglomerate (Upper Gazimur Formation) – J2; 11 – terrigene-dacite-andesite (Shadoron Formation) – J2+3; 12 – granite (Shakhtama and Asakan-Shumilovo Complexes) – J2; 13 – leucogranite (Kukulbei Complex) – J3; 14 – terrigene-volcanogenic (Turga Group) – K1; 15 – terrigenous (Kut Formation) – K1; 16 – overthrusts, upthrows and dipping angles of their fault planes; 17 – strike slip faults; 18 – zone of melanging and brecciation; 19 – high-pressure winchite-crossite facies; 20 – faults with undetermined kinematics. Faults (circled numbers): 1 – Olovyanninsky, 2 – Borzya-Gazimur, 3 – Turga-Borzya, 4 – Sherlova Gora, 5 – Norusutai-Uvyr-Nor. Tectonic plates: I – Onon-Borzya, II – Urtui, III – Kharanor, IV – Borzya. Upper Mesozoic depressions: V – Torei, VI – Ary-Bulak, VII – Turga-Kharanor. The Adun-Chelon Granite Massif–Ar. The inset is a general scheme. The Okhotsk-Mongolian Folded Zone is denoted by points, and the region considered in the paper is hatched.]()
![First thumbnail for: GEOLOGO-GEOCHEMICAL CENTRAL STRUCTURE AND METALLOG...]()
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Journal Article
Relation between cathodoluminescence and trace-element distribution of magmatic topaz from the Ary-Bulak massif, Russia Available to Purchase
Journal: Mineralogical Magazine
Published: 01 August 2016
Mineralogical Magazine (2016) 80 (5): 881–899.
...Andrea Agangi; Arnold Gucsik; Hirotsugu Nishido; Kiyotaka Ninagawa; Vadim S. Kamenetsky Abstract In order to define the cathodoluminescence (CL) properties of magmatic topaz and its relation with trace-element composition, we studied topaz phenocrysts from the Ary-Bulak ongonite massif, Russia...
FIGURES
Journal Article
Rb–Sr isotope system and Rb–Sr partitioning in the rocks of the Ary-Bulak ongonite massif, formed with the participation of fluoride–silicate magmatic immiscibility Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 November 2011
Russ. Geol. Geophys. (2011) 52 (11): 1401–1411.
...I.S. Peretyazhko; E.A. Savina; S.I. Dril’; N.S. Gerasimov Abstract The rocks of the Ary-Bulak ongonite massif (eastern Transbaikalia) have widely varying Rb (1499–4274 ppm) and Sr (10–2654 ppm) contents. In passing from porphyritic ongonites to aphyric rocks at the endocontact, Rb content increases...
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Journal Article
Fluid and magmatic processes in the formation of the Ary-Bulak ongonite massif ( eastern Transbaikalia ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 October 2010
Russ. Geol. Geophys. (2010) 51 (10): 1110–1125.
...I.S. Peretyazhko; E.A. Savina Abstract The paper discusses the formation conditions of the Ary-Bulak ongonite massif (eastern Transbaikalia). Studies of melt and fluid inclusions have shown that, along with crystalline phases and a silicate melt, ongonitic magma contained aqueous–saline fluids...
FIGURES
Image
Sr–Rb ratio in the rocks of the Ary-Bulak massif. The element contents ( Ta... Available to Purchase
in Rb–Sr isotope system and Rb–Sr partitioning in the rocks of the Ary-Bulak ongonite massif, formed with the participation of fluoride–silicate magmatic immiscibility
> Russian Geology and Geophysics
Published: 01 November 2011
Fig. 4. Sr–Rb ratio in the rocks of the Ary-Bulak massif. The element contents ( Table 1 ) were determined by double isotopic dilution; in the other cases, by ICP analysis. 1 , porphyritic ongonites; 2 , porphyritic rocks with Ca–F glass; 3 , aphyric rocks.
Image
Isochron Rb–Sr diagrams for the rocks of the Ary-Bulak massif. See descript... Available to Purchase
in Rb–Sr isotope system and Rb–Sr partitioning in the rocks of the Ary-Bulak ongonite massif, formed with the participation of fluoride–silicate magmatic immiscibility
> Russian Geology and Geophysics
Published: 01 November 2011
Fig. 6. Isochron Rb–Sr diagrams for the rocks of the Ary-Bulak massif. See description in the text.
Image
Ratios between the Sr isotope contents calculated for the rocks of the Ary-... Available to Purchase
in Rb–Sr isotope system and Rb–Sr partitioning in the rocks of the Ary-Bulak ongonite massif, formed with the participation of fluoride–silicate magmatic immiscibility
> Russian Geology and Geophysics
Published: 01 November 2011
Fig. 7. Ratios between the Sr isotope contents calculated for the rocks of the Ary-Bulak massif. See description in the text.
Image
Dependence of the measured 87 Sr/ 86 Sr ratio on the Sr content ( a ) and ... Available to Purchase
in Rb–Sr isotope system and Rb–Sr partitioning in the rocks of the Ary-Bulak ongonite massif, formed with the participation of fluoride–silicate magmatic immiscibility
> Russian Geology and Geophysics
Published: 01 November 2011
Fig. 8. Dependence of the measured 87 Sr/ 86 Sr ratio on the Sr content ( a ) and 1/Sr ( b ) of the rocks of the Ary-Bulak massif.
Image
Dependence of the initial Sr isotope ratio on the Sr content of the rocks o... Available to Purchase
in Rb–Sr isotope system and Rb–Sr partitioning in the rocks of the Ary-Bulak ongonite massif, formed with the participation of fluoride–silicate magmatic immiscibility
> Russian Geology and Geophysics
Published: 01 November 2011
Fig. 9. Dependence of the initial Sr isotope ratio on the Sr content of the rocks of the Ary-Bulak massif. 1 , 2 , rocks of the massif; 3 , 4 , 87 Sr/ 86 Sr in the limestones of the Ust’-Borzya Formation ( 1 , 4 , authors’ data; 2 , 3 , after ( Kostit-syn et al., 2004 )).
Image
![Normalized [20] REE patterns of granites of the Khangilai intrusion. Granites: 1 — MIP biotite granites, 2 — muscovite granites of exocontact dikes of the Spokoiny dome, 3 — muscovite granites of the Khangilai massif, 4 — granite-porphyries of the Ubzhigoi series, 5 — intensely greisenized muscovite granites of the Spokoiny dome, 6 — amazonite Li-F-granites of the Orlovka dome, 7 — ongonites of the Ary-Bulak massif (Sherlovaya Gora area). The curve numbers correspond to the run numbers in Table 2.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/rgg/46/5/rgg-460486/2/s_s02may05_page_12_1.jpeg?Expires=2147483647&Signature=DwtIjgnx5wRYR0Pyw0hYeesrySZMdu57E0EIHd3FhUzcq7-NO4Sd0DC6jLdhc5fSxgg-nxYWZTBrrhmD-As~WaDPYpA23bhLvTGFnwojPF7k9FrZdfcmXV6B-gXtUNWil1ft9rZFFi4l4AIj5YkoVXjqDUJ09iWlABytMYO3kLc4cN6jiTFxS~Ev8EK60S7cYM951jEkih5wTS~3C60Ls-cAtR69ign3lAbKZJURfCPDioR3Cmoh~snaadgFYj5PLxh3n8euw6iL5t1Wmlwk6rOkYzGxU6iXHcRcIoUakpiw-Bqco2Y1B8~3GU~ZDTnJy2L5NVzyjLjcsG~uF4~~JA__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Normalized [ 20 ] REE patterns of granites of the Khangilai intrusion. Gran... Available to Purchase
in GEOLOGO-GEOCHEMICAL CENTRAL STRUCTURE AND METALLOGENY OF GRANITE ORE-MAGMATIC SYSTEMS IN EASTERN TRANSBAIKALIA
> Russian Geology and Geophysics
Published: 01 May 2005
— intensely greisenized muscovite granites of the Spokoiny dome, 6 — amazonite Li-F-granites of the Orlovka dome, 7 — ongonites of the Ary-Bulak massif (Sherlovaya Gora area). The curve numbers correspond to the run numbers in Table 2 .
Image
Calcium fluoride phase (partly crystalline glass) in the Ca- and F-enriched... Available to Purchase
in Fluid and magmatic processes in the formation of the Ary-Bulak ongonite massif ( eastern Transbaikalia )
> Russian Geology and Geophysics
Published: 01 October 2010
Fig. 1. Calcium fluoride phase (partly crystalline glass) in the Ca- and F-enriched rocks of the Ary-Bulak massif. a , Large segregations of the calcium fluoride phase (black areas) in Ca- and F-rich porphyritic rock (sample ARB131), viewed under ×-polars; b , groundmass (sample ARB148); c
Journal Article
Melts and fluids in natural mineral and ore formation: modern studies of fluid and melt inclusions in minerals Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 November 2011
Russ. Geol. Geophys. (2011) 52 (11): 1283–1285.
...–1747).
Peretyazhko , I.S. , Savina , E.A. , Dril’ , S.I. , Gerasimov , N.S. , 2011 . Rb–Sr isotope system and Rb–Sr partitioning in the rocks of the Ary-Bulak ongonite massif, formed with the participation of fluoride–silicate magmatic...
Journal Article
The fingerprint of imperial topaz from Ouro Preto region (Minas Gerais state, Brazil) based on cathodoluminescence properties and composition Available to Purchase
Journal: Mineralogical Magazine
Published: 28 February 2018
Mineralogical Magazine (2018) 82 (4): 943–960.
.... , 2013 ); and F-rich ongonites from Ary-Bulak massif, Russia (Agangi et al. , 2014 , 2016 ). Table 3. Comparison between the trace-element composition of imperial topaz and topaz crystals from different geological environments (ppm). Environment Ti V Cr Mn Fe Cu Zn Ga Ge...
FIGURES
Journal Article
Ongonite–elvan magmas of the Kalguty ore-magmatic system ( Gorny Altai ): composition, fluid regime, and genesis Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 November 2011
Russ. Geol. Geophys. (2011) 52 (11): 1378–1400.
... of ongonites in the Ary-Bulak Massif, eastern Transbaikalia . Petrology 17 ( 6 ), 558 – 569 .
Barnes , H.L.
(Ed.), 1979 . Solubility of ore minerals , in: Geochemistry of Hydrothermal Ore Deposits , Wiley , New York , pp. 404 – 460...
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Journal Article
THE EAST-TRANSBAIKALIAN COVER-FOLDED ARCH Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 June 1996
Russ. Geol. Geophys. (1996) 37 (6): 59–66.
... (circled numbers): 1 – Olovyanninsky, 2 – Borzya-Gazimur, 3 – Turga-Borzya, 4 – Sherlova Gora, 5 – Norusutai-Uvyr-Nor. Tectonic plates: I – Onon-Borzya, II – Urtui, III – Kharanor, IV – Borzya. Upper Mesozoic depressions: V – Torei, VI – Ary-Bulak, VII – Turga-Kharanor. The Adun-Chelon Granite Massif–Ar...
FIGURES
Image
A structural scheme of the East-Transbaikalian Cover-Folded Arch. Complexes... Available to Purchase
Published: 01 June 1996
numbers): 1 – Olovyanninsky, 2 – Borzya-Gazimur, 3 – Turga-Borzya, 4 – Sherlova Gora, 5 – Norusutai-Uvyr-Nor. Tectonic plates: I – Onon-Borzya, II – Urtui, III – Kharanor, IV – Borzya. Upper Mesozoic depressions: V – Torei, VI – Ary-Bulak, VII – Turga-Kharanor. The Adun-Chelon Granite Massif–Ar. The inset
Journal Article
The seismic signal strength of chemical explosions Available to Purchase
Publisher: Seismological Society of America
Published: 01 December 1998
Bulletin of the Seismological Society of America (1998) 88 (6): 1511–1524.
....
(1995) .
Study of underground mining explosions in the Khibiny massif ,
NORSAR Sci. Report 2-94/95 ,
137 -
149 .
Latter
A.
(1960) .
Decoupling of underground explosions , in
Project VELA, Proceedings of a Symposium ,
160...
Journal Article
GEOLOGO-GEOCHEMICAL CENTRAL STRUCTURE AND METALLOGENY OF GRANITE ORE-MAGMATIC SYSTEMS IN EASTERN TRANSBAIKALIA Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2005
Russ. Geol. Geophys. (2005) 46 (5): 486–503.
... — intensely greisenized muscovite granites of the Spokoiny dome, 6 — amazonite Li-F-granites of the Orlovka dome, 7 — ongonites of the Ary-Bulak massif (Sherlovaya Gora area). The curve numbers correspond to the run numbers in Table 2 . ...
FIGURES
Journal Article
Changes in the Ta/Nb Ratio in Successively Formed Differentiates of Granite Melt (Calculations Based on Experimental Data) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 2020
Russ. Geol. Geophys. (2020) 61 (1): 26–35.
... of the Ary-Bulak ongonite massif (eastern Transbaikalia) . Russian Geology and Geophysics (Geologiya i Geofizika) 51 ( 10 ), 1110 – 1125 (1423–1442) .
Peretyazhko , I.S. , Savina , E.A. , Dril’ , S.I. , Gerasimov , N.S. , 2011 . Rb– Sr...
FIGURES
Journal Article
Stages and Duration of Formation of the Kalguty Mo–W Ore-Magmatic System (Altai): Thermochronology and Mathematical Modeling Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 August 2019
Russ. Geol. Geophys. (2019) 60 (8): 890–910.
... . Geochemical specifics of ongonites in the Ary-Bulak massif, eastern Transbaikalia . Petrology 17 ( 6 ), 558 – 569 .
Antipin , V.S. , Perepelov , A.B. , Ochir , G. , Odgerel , D. , Tsegmed , Z. , 2016 . Late Paleozoic and Early Mesozoic...
FIGURES
Journal Article
EARLY CRETACEOUS GRANITOIDS OF THE SOKTUI MASSIF: COMPOSITION AND PETROGENESIS ( eastern Transbaikalia ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2025
Russ. Geol. Geophys. (2025) 66 (5): 570–592.
... system and Rb–Sr partitioning in the rocks of the Ary-Bulak ongonite massif, formed with the participation of fluoride–silicate magmatic immiscibility . Russian Geology and Geophysics 52 ( 11 ), 1401 – 1411 , DOI: 10.1016/j.rgg.2011.10.009 . Pitzer , K.S. , Pabalan , R.T. ( 1986...
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