Search Results - "Busharina, S. V."

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  1. 1

    Sources of Zircons from Clastic Rocks of the Riphean Sequences of the Urals by Krasnobaev, A. A., Puchkov, V. N., Sergeeva, N. D., Busharina, S. V.

    Published in Doklady earth sciences (01-10-2019)
    “…New dates of detrital zircons from sandstones expand the possibilities to interpret their source areas. These interpretations are often constrained by a formal…”
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  2. 2

    U–Pb (SHRIMP) Zircon Age of Granitoid Pebbles from the Kukkarauk Conglomerates of the Vendian Asha Group (Alatau Anticlinorium, Southern Urals) by Krasnobaev, A. A., Puchkov, V. N., Sergeeva, N. D., Busharina, S. V.

    Published in Doklady earth sciences (01-06-2019)
    “…Abstraсt The lack of reliable geochronological data for the Vendian deposits of the Urals and other regions is one reason why there is still uncertainty in the…”
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  3. 3

    Zirconology of rutile eclogites of the Maksutov Complex (Southern Urals) by Krasnobaev, A. A., Valizer, P. M., Anfilogov, V. N., Medvedeva, E. V., Busharina, S. V.

    Published in Doklady earth sciences (01-11-2017)
    “…The age data (U–Pb, SHRIMP II) of zircons from rutile eclogites of the Maksutov Complex (MC) (village Shubino, Southern Urals) were subdivided into three age…”
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  4. 4

    Mineralogy, U–Pb (TIMS, SHRIMP) age, and rare-earth elements in zircons from granites of the Mazara Massif, South Urals by Krasnobaev, A. A., Puchkov, V. N., Sergeeva, N. D., Busharina, S. V.

    Published in Geochemistry international (01-06-2017)
    “…The paper reports the results of mineralogical, geochemical, and geochronological (TIMS and SHRIMP) study of heterogeneous zircons from granites of the Mazara…”
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  5. 5

    Zircons, age, and geological setting of rhyodacite–porphyry from the Bagrusha Complex (South Urals) by Puchkov, V. N., Krasnobaev, A. A., Sergeeva, N. D., Busharina, S. V., Shokalsky, S. P.

    Published in Doklady earth sciences (01-11-2017)
    “…Before our studies, it was considered that the Bagrusha rhyolite–porphyry complex (BC) including veins and thin dykes occurring in the Kusa region among…”
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  6. 6

    Zircons in Gabbro of the Nurali Massif (Southern Ural) by Krasnobaev, A. A., Valizer, P. M., Anfilogov, V. N., Medvedeva, E. V., Busharina, S. V.

    Published in Doklady earth sciences (01-06-2018)
    “…The formation time of 410.5 ± 1.1 Ma (zircon U/Pb SHRIMP) and the duration of rock crystallization (2–2.5 Ma) were determined for gabbro from the Nurali…”
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  7. 7

    Zirconology of miaskites from the Ilmeny Mountains, South Urals by Krasnobaev, A. A., Valizer, P. M., Busharina, S. V., Medvedeva, E. V.

    Published in Geochemistry international (01-09-2016)
    “…It is shown that the replacement and long evolution of miaskitic zircons led to the formation of two main age groups: 420–380 Ma (I) and 260–240 Ma (II). The…”
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  8. 8

    Polychronous zirconology of syenites from the Avashla intrusion in the Kurgass anticline (Southern Urals) by Krasnobaev, A. A., Puchkov, V. N., Sergeeva, N. D., Shokalski, S. P., Busharina, S. V.

    Published in Doklady earth sciences (01-03-2017)
    “…Zircons were separated from syenites of the Avashla intrusion in the Kurgass anticline of the Bashkir megaanticlinorium in the Southern Urals. The obtained…”
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  9. 9

    Zirconology of Navysh volcanic rocks of the Ai Suite and the problem of the age of the Lower Riphean boundary in the Southern Urals by Krasnobaev, A. A., Puchkov, V. N., Kozlov, V. I., Sergeeva, N. D., Busharina, S. V., Lepekhina, E. N.

    Published in Doklady earth sciences (01-02-2013)
    “…Volcanic rocks of the Navysh Complex occur in the base of the Lower Riphean Ai Formation of the Burzyan Series within the Bashkirian meganticlinorium. The…”
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  10. 10

    Zirconology of lherzolites in the Nurali Massif by Krasnobaev, A. A., Rusin, A. I., Anfilogov, V. N., Valizer, P. M., Busharina, S. V., Medvedeva, E. V.

    Published in Doklady earth sciences (01-06-2017)
    “…The age trend (SHRIMP U/Pb) of the evolution of zircon is obtained for the first time in lherzolites of the Nurali Massif. Zircons are subdivided into groups…”
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  11. 11

    Zirconology of serpentinites from Nyashevo massif (Southern Urals) by Krasnobaev, A. A., Valizer, P. M., Anfilogov, V. N., Medvedeva, E. V., Busharina, S. V., Murdasova, N. M.

    Published in Doklady earth sciences (01-12-2016)
    “…Zircons in serpentinites from Nyashevo massif of the Ilmenogorskii complex were dated for the first time by means of the SHRIMP technique. The maximum date of…”
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  12. 12

    Zircon geochronology of the Mashak volcanic rocks and the problem of the age of the lower-middle Riphean boundary (Southern Urals) by Krasnobaev, A. A., Kozlov, V. I., Puchkov, V. N., Busharina, S. V., Sergeeva, N. D., Paderin, I. P.

    Published in Stratigraphy and geological correlation (01-09-2013)
    “…In the type sections of the Riphean within the Bashkirian mega-anticlinorium (Southern Urals), the Mashak Formation represents a basal unit of the Middle…”
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  13. 13

    Uranium-lead age of zircons from granites and the substrate of the Mazara massif (Southern Urals) by Krasnobaev, A. A., Puchkov, V. N., Sergeeva, N. D., Busharina, S. V.

    Published in Doklady earth sciences (01-07-2015)
    “…The U–Pb dating of zircons from the Mazara granite massif (Southern Urals) by means of the SHRIMP II technique resulted in the conclusion that the zircons were…”
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  14. 14

    Zirconology of garnet-glaucophane schists of the Maksyutov complex (Southern Urals) by Krasnobaev, A. A., Valizer, P. M., Anfilogov, V. N., Busharina, S. V.

    Published in Doklady earth sciences (01-04-2015)
    “…Abstarct The studies of zircons from garnet-glaucophane schists of the Maksyutov complex (Novotashlinskii area) have shown that their substrate was constituted…”
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  15. 15

    Zirconology of ultrabasic rocks of the Karabash massif (Southern Urals) by Krasnobaev, A. A., Valizer, P. M., Anfilogov, V. N., Sergeev, S. A., Rusin, A. I., Busharina, S. V., Medvedeva, E. V.

    Published in Doklady earth sciences (01-07-2016)
    “…Dating of zircon (SHRIMP) from dunite and harzburgite of the Karabash massif was carried out for the first time. Relics of ancient crystals (1940 ± 30 Ma in…”
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  16. 16

    First U–Pb isotopic data on zircon from andesite of the Saf’yanovka Cu-bearing massive sulfide deposit (Middle Urals) by Ronkin, Yu. L., Pritchin, M. E., Soroka, E. I., Gerdes, A., Puchkov, V. N., Busharina, S. V.

    Published in Doklady earth sciences (01-07-2016)
    “…New results of U–Pb LA ICP–MS dating of zircon from andesite samples cropping out on the western wall of the Saf’yanovka quarry (57°22′58.88″ N, 61°31′50.85″…”
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  17. 17

    Zircon Archean of the Transuralian megazone by Krasnobaev, A. A., Puchkov, V. N., Puzhakov, B. A., Busharina, S. V., Sergeeva, N. D.

    Published in Doklady earth sciences (01-12-2015)
    “…The Il’inka metamorphic complex (IC) is located in the Transuralian megazone at the latitude of the Chelyabinsk granite pluton, east of the Chelyabinsk graben…”
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  18. 18

    Zirconology of ultrabasic rocks of the Buldym massif (Il’meno-Vishnevogorskii Complex, Southern Urals) by Krasnobaev, A. A., Valizer, P. M., Rusin, A. I., Busharina, S. V., Medvedeva, E. V.

    Published in Doklady earth sciences (01-03-2015)
    “…The Buldym massif (BM) of ultrabasic rocks occurs among metamorphic rocks of the Precambrian Vishnevogorskaya Suite (Fig. 1) in the northern part of the…”
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  19. 19

    Zirconology of ultramafic rocks from the Vostochnotagilskii massif (Middle Urals) by Krasnobaev, A. A., Rusin, A. I., Busharina, S. V., Rodionov, N. V.

    Published in Doklady earth sciences (01-04-2014)
    “…The Vostochnotagilskii massif (VTM; also known as Krasnouralskii) is one of the largest in the Middle and North Urals. This massif occurs in the meridian…”
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  20. 20

    Zirconology of pegmatites of the Ilmeny Mountains by Krasnobaev, A. A., Valizer, P. M., Anfilogov, V. N., Nemov, A. B., Busharina, S. V.

    Published in Doklady earth sciences (01-08-2014)
    “…Zircons extracted from the nepheline and feldspar crystals of miaskitic and feldspar pegmatites, respectively, are analyzed with the SHRIMP method for the…”
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