Paleozoic stage formation of the alkaline rocks massif Bogdo, Arctic Siberia (by 40Ar/39Ar dating)

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Abstract

The age of potassium-bearing minerals from high-K nepheline syenites, libeneritized and carbonatized nepheline syenites, as well as pseudoleucite syenites of the Bogdo alkaline massif (Arctic Siberia) was determined by the 40Ar/39Ar method. As a result of generalization and analysis of the 40Ar/39Ar dating data, on the summary thermochronological diagram for minerals from the rocks of the Tomtor massif, the Udachnaya-Vostochnaya kimberlite pipe, and alkaline rocks of the Bogdo massif, the polychronicity of the formation of alkaline complexes of the Tomtor type at the Paleozoic stage was revealed. Based on isotopic data, a complex, three-stage history of the formation of the rocks of the Bogdo massif is reconstructed, with the manifestation of the Late Devonian-Early Carboniferous stage – the most productive for rare-metal-rare-earth mineralization. The Devonian period of the formation of the Tomtor and Bogdo massifs is associated with the impact of the Vilyui plume on the eastern edge of the Siberian craton. A close age interval is fixed during the formation of the rocks of the Kola alkaline province.

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S. M. Zhmodik

V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Author for correspondence.
Email: zhmodik@igm.nsc.ru
Russian Federation, Novosibirsk

A. V. Travin

V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: zhmodik@igm.nsc.ru
Russian Federation, Novosibirsk

E. V. Lazareva

V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: zhmodik@igm.nsc.ru
Russian Federation, Novosibirsk

D. S. Yudin

V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: zhmodik@igm.nsc.ru
Russian Federation, Novosibirsk

D. K. Belyanin

V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: zhmodik@igm.nsc.ru
Russian Federation, Novosibirsk

A. V. Tolstov

V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: zhmodik@igm.nsc.ru
Russian Federation, Novosibirsk

N. N. Dobretsov

V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: zhmodik@igm.nsc.ru
Russian Federation, Novosibirsk

References

  1. Эрлих Э. Н. Новая провинция щелочных пород на севере Сибирской платформы // ЗВМИ. 1964. Ч. XCIII. Вып. 6. С. 682–693.
  2. Зайцев А. И., Энтин А. Р., Ненашев Н. И., Лазебник К. А., Тян О. А. Геохронология и изотопная геология Якутии. Якутск: ЯНЦ СО РАН, 1992. 248 с.
  3. Владыкин Н. В., Котов А. Б., Борисенко А. С., Ярмолюк В. В., Похиленко Н. П., Сальникова Е. Б., Травин А. В., Яковлева С. З. Возрастные рубежи формирования щелочно-ультраосновного массива Томтор: результаты геохронологических U-Pb- и A 40 r/ A 39 r-исследований // ДАН. 2014. Т. 454. № 2. С. 195–199.
  4. Dobretsov N. L., Zhmodik S. M., Lazareva E. V., Tolstov A. V., Belyanin D. K., Surkov O. N., Dobretsov N. N., Rodionov N. V., Sergeev S. A. U–Pb Age of Sphene and the Petrochemical, Mineralogical, and Geochemical Features of Alkaline Rocks of the Bogdo Complex (Arctic Siberia) // Doklady Earth Sciences. 2019. V. 489. Part 1. P. 1352–1357.
  5. Травин А. В., Юдин Д. С., Владимиров А. Г., Хромых С. В., Волкова Н. И., Мехоношин А. С., Колотилина Т. Б. Термохронология Чернорудской гранулитовой зоны (Ольхонский регион, Западное Прибайкалье) // Геохимия. 2009. Т. 11. С. 1181–1199.
  6. Ludwig K. R. ISOPLOT/Ex A geochronological toolkit for Microsoft Excel, Version 3.6 // Berkeley Geochronology Center Special Publication. № 4. 2008. 76 p.
  7. Moller W., Williams-Jones A. E. Petrogenesis of the Nechalacho Layered Suite, Canada: Magmatic Evolution of a REE–Nb-rich Nepheline Syenite Intrusion // Journal of Petrology. 2016. V. 57. No 2. P. 229–276.
  8. Hodges K. V. Geochronology and Thermochronology in Orogenic Systems // In: Treatise on Geochemistry. Oxford: Elsevier, 2004. P. 263–292.
  9. Юдин Д. С., Томиленко А. А., Травин А. В., Агашев А. М., Похиленко Н. П., Орихаши Ю. Возраст внедрения кимберлитовой трубки Удачная-Восточная: U/Pb- и A 40 r/ A 39 r-данные // ДАН. 2014. Т. 455. № 1. С. 91–93.
  10. Добрецов Н. Л., Лазарева Е. В., Жмодик С. М., Пономарчук В. А., Травин А. В., Мягкая И. Н., Толстов А. В., Карманов Н. С. Ультракалиевая порода Томторского комплекса щелочных пород и карбонатитов (Арктическая Сибирь) // ДАН. 2020. Т. 495. № 2. С. 23–27.
  11. Spetsius Z. V., Belousova E. A., Griffin W. L., O’Reilly S.Y., Pearson N. J. Archean sulfide inclusions in Paleozoic zircon megacrysts from the Mir kimberlite, Yakutia: implications for the dating of diamonds // Earth and Planetary Science Letters. 2002. V. 199. № 1–2. P. 111–126.
  12. Резвухин Д. И. Гранаты с минеральными включениями оксидов и сульфидов из кимберлитовой трубки Интернациональная: минералогия, геохимия и связь с процессами мантийного метасоматоза в литосферной мантии Мирнинского поля, Сибирский кратон. Дисс. к. г.- м. н. Новосибирск: ИГМ СО РАН. 2016. 173 с.
  13. Kramm U., Kogarko L. N. Nd and Sr isotope signatures of the Khibina and Lovozero agpaitic centres, Kola Alkaline Province, Russia // Lithos. 1994. V. 32. P. 225–242.
  14. Арзамасцев А. А., Арзамасцева Л. В., Травин А. В., Беляцкий Б. В., Шаматрина А. М., Антонов А. В., Ларионов А. Н., Родионов Н. В., Сергеев С. А. Длительность формирования палеозойской магматической системы в центральной части Кольского полуострова: U-Pb-, Rb-Sr-, Ar-Ar-данные // ДАН 2007. Т. 417. № 5. С. 666–670.
  15. Стифеева М. В., Сальникова Е. Б., Арзамасцев А. А., Котов А. Б., Гроздев В. Ю. Кальциевые гранаты как источник информации о возрасте щелочно-ультраосновных интрузий Кольской магматической провинции // Петрология. 2020. Т. 28. № 1. С. 72–84.
  16. Bulakh A. G., Le Bas M. J., Wall F., Zaitsev A. N. Ancylite-bearing carbonatites of the Seblyavr massif, Kola peninsula, Russia // Neues Jahrbuch für Mineralogie, Monatshefte. 1998. 171–192.
  17. Агеева О. А. Типоморфизм акцессорных минералов и эволюция минералообразования в породах комплекса рисчорритов: Хибинский массив. Дисс. к. г.- м. н. 2002. М.: ИГЕМ. 187 с.
  18. Irber W. The lanthanide tetrad effect and its correlation with K/Rb, Eu/Eu*, Sr/Eu, Y/Ho, and Zr/Hf of evolving peraluminous granite suites // Geochim. Cosmochim. Acta 1999. V. 63. No. ¾. P. 489–508.
  19. McDonough W. F., Sun S.-s. The composition of the Earth // Chemical Geology. 1995.V. 120. P. 223–253.
  20. Arzamastsev A. A., Bea F., Glaznev V. N., Arzamastseva L. V., Montero L. V. Kola alkaline province in the Paleozoic evaluation of primary mantle magma composition and magma generation conditions // Russian Journal of Earth Sciences. 2002. V. 3. Nо 1. P. 1–32.

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2. Fig. 1. General view (a, c, d, g) and microphotographs (b, d, f, h) of rocks of the Bogdo alkaline massif, for which the 40Ar/39Ar age was determined for Bi, Neph and KPSh. a–b – Bog-18 – VKNS (rischorrite); c–g – Bog-6 m/z-sr/z libenerite nepheline syenites (LNS); d–f – Bog-14 m/z-kr/z libenerite nepheline syenites (LNS); g–h – Bog-1 – pleudoleucite carbonated syenite (PLCS). Aeg – Aegirine; Bt – Biotite; Cat – Calcite; Ml – Melanite; Ttn – Titanite; Fsp – K-feldspar; Ap – Apatite; Nph – Nepheline; Lib – Libenerite.

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3. Fig. 2. SiO2–Na2O+K2O diagram for rocks of the Bogdo massif (1 – LNS; 2 – VKNS; 3 – PLKS) and 4 – Nechalacho Layered Suite, according to [7].

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4. Fig. 3. Age 40Ar/39Ar spectra for minerals from alkaline rocks of the Bogdo massif. Mineral fractions are shown in color: 1 – biotite, 2 – nepheline, 3 – KPSh. Bog-1, Bog-6, Bog-14, Bog-18 – see Table 1.

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5. Fig. 4. Summary thermochronological diagram (Paleozoic stage) for minerals from the rocks of the Tomtor massif [3, 4] and the Udachnaya-Vostochnaya kimberlite pipe (U-V with a light background) [9] (top); for alkaline rocks of the Bogdo massif (bottom). U/Pb dating of titanite is given according to [4].

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6. Fig. 5. Diagrams demonstrating the dependencies of variations in the degree of the tetrad effect: REE, normalized by chondrite C1 [19] (1 - Bog-1; 2 - Bog-6; 3 - Bog-14; 4 - Bog-18; 5 - VKNS (average for samples 455/890 and 818/637) of the Khibiny massif, after [20]); TE3 - Gd-Ho) and Lan/Ndn; K2O (wt.%); BaO (wt.%) for the rocks of the Bogdo massif. 1 - pseudoleucite syenites; 2 - VKNS; 3–6 - LS; 6 - PLKS.

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