Sulfides in the marbles of spurrite-merwinite facies: the Kochumdek River, East Siberia

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Abstract


In the marbles of the Kochumdek contact metamorphic aureole pyrrhotite, rasvumite, sphalerite, alabandite, wurtzite, galena, acanthite have been identified. Mineralogical diversity of sulphides is the consequence of the efficient crystal-chemical fractionation of trace elements under the PT‑conditions of spurrite-merwinite metamorphic facies. Trace element and isotope fingerprints of sulfides indicate that sedimentary parent rocks were the main source of sulfur and metals for sulfides mineralization.


About the authors

E. V. Sokol

Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Author for correspondence.
Email: sokol@igm.nsc.ru

Russian Federation, 3, Koptyug prospect, Novosibirsk, 630090

A. S. Deviatiiarova

Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: sokol@igm.nsc.ru

Russian Federation, 3, Koptyug prospect, Novosibirsk, 630090

S. N. Kokh

Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: sokol@igm.nsc.ru

Russian Federation, 3, Koptyug prospect, Novosibirsk, 630090

V. V. Reverdatto

Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences

Email: sokol@igm.nsc.ru

Russian Federation, 3, Koptyug prospect, Novosibirsk, 630090

Academician of the Russian Academy of Sciences

D. A. Artemyev

South Ural Federal Research Center of Mineralogy and Ecology, Ural Branch of the Russian Academy of Sciences; "South Ural State University" (national research university)

Email: sokol@igm.nsc.ru

Russian Federation, Ilmeny Reserve, Miass, Chelyabinsk district, 456317; 76, Lenin prospekt, Chelyabinsk, 454080

V. Yu. Kolobov

Publishing House of Siberian Branch of the Russian Academy of Sciences

Email: sokol@igm.nsc.ru

Russian Federation, 2, Morskoy avenue, Novosibirsk, 630090

References

  1. Slotznick S. P., Eiler J. M., Fischer W. W. // Geochim et Cosmochim Acta. 2018. V. 224 (5). P. 96-115.
  2. Vaughan D. J. (Ed.) Sulfide Mineralogy and Geochemistry. Series. Reviews in mineralogy. Geochem. Soc. and Mineral. Soc. America. Washington D. C. 2006. V. 61. 714 p.
  3. Ревердатто В. В. Фации контактового метаморфизма. М.: Недра, 1970. 271 с.
  4. Перцев Н. Н. Высокотемпературный метаморфизм и метасоматоз карбонатных пород. М.: Наука, 1977. 256 с.
  5. Сокол Э. В., Полянский О. П., Семенов А. Н., Ревердатто В. В., Кох С. Н., Девятиярова А. С., Колобов В. Ю., Хворов П. В., Бабичев А. В. // Геология и геофизика. 2019. Т. 60. № 4. С. 456-471.
  6. Артемьев Д. А., Масленников В. В., Филиппова К. А. // Металлогения древних и современных океанов - 2017. Дифференциация и причины разнообразия рудных месторождений. Миасс: ИМин УрО РАН, 2017. С. 201-206.
  7. Gerasimova Y. V., Oreshonkov A. S., Romanova O. B., Ivanenko A. A., Krylov A. S. // J. Spectrosc. Lett. 2017. V. 50 (1). P. 55-58.
  8. Lin Y., Goresy A. E. // Meteoritics and Planet. Sci. 2002. V. 37 (4). P. 577-599.
  9. Osadchii E. G., Gorbaty Y. E. // Geochim et Cosmochim Acta. 2010. V. 74 (2). P. 568-573.
  10. Scocioreanu M., Baibarac M., Baltog I., Pasuk I., Velula T. // J. Solid State Chem. 2012. V. 186. P. 217-223.
  11. Добровольская М. Г. Сульфиды щелочных металлов в природе. М.: Наука, 2018. 159 с.
  12. Pekov I. V., Agakhanov A. A., Boldyreva M. M., Grishin V. G. // Canad. Miner. 2005. V. 43 (3). P. 965-972.
  13. Golovin A. V., Goryainov S. V., Kokh S. N., Sharygin I. S., Rashchenko S. V., Kokh K. A., Sokol E. V., Devyatiyarova A. S. // J. Raman spectrosc. 2017. V. 48. P. 1574-1582.
  14. Ye L., Cook N. J., Ciobanu C. L., Yuping L., Qian Z., Tiegeng L., Wei G., Yulong Y., Danyushevskiy L. // Ore Geology Reviews. 2011. V. 39 (4). P. 188-217.
  15. Osadchii V. O., Voronin M. V., Baranov A. V. // Contribs to Mineral. and Petrol. 2018. V. 173. P. 1-9.

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