Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia

D. I. Rezvukhin, V. G. Malkovets, I. S. Sharygin, D. V. Kuzmin, A. A. Gibsher, K. D. Litasov, N. P. Pokhilenko, N. V. Sobolev

    Research output: Contribution to journalArticle

    3 Citations (Scopus)

    Abstract

    The results of study of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe are reported. Most of the studied samples are characterized by high concentrations of Sr, Ca, Na, and LREEs in comparison with minerals of the LIMA series from kimberlites of South Africa, whereas the average concentrations of Ba and K are significantly lower. Crichtonite group minerals in pyropes are characterized by predomination of Na over K in most samples and by a high concentration of Al2O3 (up to 4.5 wt %). Findings of inclusions of crichtonite group minerals with high concentrations of incompatible elements provide evidence for the metasomatic origin of host chromium-rich pyropes.

    Original languageEnglish
    Pages (from-to)206-209
    Number of pages4
    JournalDoklady Earth Sciences
    Volume466
    Issue number2
    DOIs
    Publication statusPublished - Feb 1 2016

    Fingerprint

    pyrope
    kimberlite
    pipe
    mineral
    chromium

    ASJC Scopus subject areas

    • Earth and Planetary Sciences (miscellaneous)
    • Earth and Planetary Sciences(all)

    Cite this

    Rezvukhin, D. I., Malkovets, V. G., Sharygin, I. S., Kuzmin, D. V., Gibsher, A. A., Litasov, K. D., ... Sobolev, N. V. (2016). Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. Doklady Earth Sciences, 466(2), 206-209. https://doi.org/10.1134/S1028334X16020227

    Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. / Rezvukhin, D. I.; Malkovets, V. G.; Sharygin, I. S.; Kuzmin, D. V.; Gibsher, A. A.; Litasov, K. D.; Pokhilenko, N. P.; Sobolev, N. V.

    In: Doklady Earth Sciences, Vol. 466, No. 2, 01.02.2016, p. 206-209.

    Research output: Contribution to journalArticle

    Rezvukhin, DI, Malkovets, VG, Sharygin, IS, Kuzmin, DV, Gibsher, AA, Litasov, KD, Pokhilenko, NP & Sobolev, NV 2016, 'Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia', Doklady Earth Sciences, vol. 466, no. 2, pp. 206-209. https://doi.org/10.1134/S1028334X16020227
    Rezvukhin DI, Malkovets VG, Sharygin IS, Kuzmin DV, Gibsher AA, Litasov KD et al. Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. Doklady Earth Sciences. 2016 Feb 1;466(2):206-209. https://doi.org/10.1134/S1028334X16020227
    Rezvukhin, D. I. ; Malkovets, V. G. ; Sharygin, I. S. ; Kuzmin, D. V. ; Gibsher, A. A. ; Litasov, K. D. ; Pokhilenko, N. P. ; Sobolev, N. V. / Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. In: Doklady Earth Sciences. 2016 ; Vol. 466, No. 2. pp. 206-209.
    @article{315d961920084ce981e00d583fe97d8c,
    title = "Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia",
    abstract = "The results of study of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe are reported. Most of the studied samples are characterized by high concentrations of Sr, Ca, Na, and LREEs in comparison with minerals of the LIMA series from kimberlites of South Africa, whereas the average concentrations of Ba and K are significantly lower. Crichtonite group minerals in pyropes are characterized by predomination of Na over K in most samples and by a high concentration of Al2O3 (up to 4.5 wt {\%}). Findings of inclusions of crichtonite group minerals with high concentrations of incompatible elements provide evidence for the metasomatic origin of host chromium-rich pyropes.",
    author = "Rezvukhin, {D. I.} and Malkovets, {V. G.} and Sharygin, {I. S.} and Kuzmin, {D. V.} and Gibsher, {A. A.} and Litasov, {K. D.} and Pokhilenko, {N. P.} and Sobolev, {N. V.}",
    year = "2016",
    month = "2",
    day = "1",
    doi = "10.1134/S1028334X16020227",
    language = "English",
    volume = "466",
    pages = "206--209",
    journal = "Doklady Earth Sciences",
    issn = "1028-334X",
    publisher = "Maik Nauka-Interperiodica Publishing",
    number = "2",

    }

    TY - JOUR

    T1 - Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia

    AU - Rezvukhin, D. I.

    AU - Malkovets, V. G.

    AU - Sharygin, I. S.

    AU - Kuzmin, D. V.

    AU - Gibsher, A. A.

    AU - Litasov, K. D.

    AU - Pokhilenko, N. P.

    AU - Sobolev, N. V.

    PY - 2016/2/1

    Y1 - 2016/2/1

    N2 - The results of study of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe are reported. Most of the studied samples are characterized by high concentrations of Sr, Ca, Na, and LREEs in comparison with minerals of the LIMA series from kimberlites of South Africa, whereas the average concentrations of Ba and K are significantly lower. Crichtonite group minerals in pyropes are characterized by predomination of Na over K in most samples and by a high concentration of Al2O3 (up to 4.5 wt %). Findings of inclusions of crichtonite group minerals with high concentrations of incompatible elements provide evidence for the metasomatic origin of host chromium-rich pyropes.

    AB - The results of study of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe are reported. Most of the studied samples are characterized by high concentrations of Sr, Ca, Na, and LREEs in comparison with minerals of the LIMA series from kimberlites of South Africa, whereas the average concentrations of Ba and K are significantly lower. Crichtonite group minerals in pyropes are characterized by predomination of Na over K in most samples and by a high concentration of Al2O3 (up to 4.5 wt %). Findings of inclusions of crichtonite group minerals with high concentrations of incompatible elements provide evidence for the metasomatic origin of host chromium-rich pyropes.

    UR - http://www.scopus.com/inward/record.url?scp=84962762010&partnerID=8YFLogxK

    UR - http://www.scopus.com/inward/citedby.url?scp=84962762010&partnerID=8YFLogxK

    U2 - 10.1134/S1028334X16020227

    DO - 10.1134/S1028334X16020227

    M3 - Article

    VL - 466

    SP - 206

    EP - 209

    JO - Doklady Earth Sciences

    JF - Doklady Earth Sciences

    SN - 1028-334X

    IS - 2

    ER -