To the origin of the fluorite of the Sushchany-Perga ore zone (Ukrainian Shield)

1Ponomarenko, OM, Voznyak, DK, Samchuk, AI, Belskyy, VM
1M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine, Kyiv
Dopov. Nac. akad. nauk Ukr. 2017, 11:52-58
Section: Geosciences
Language: Ukrainian

Precambrian shields are characterized by channels, through which the matter and heat of the mantle flow into the Earth's crust. They are zones of deep faults, kimberlite pipes, volcanoes, and other disjunctive dislocations. Peridotite, kimberlite, lamproite, and other rocks indicate the mantle origin. If igneous rocks do not cause objections to their mantle origin, the relationship of juvenile fluids that appear in the zone of deep faults with the mantle requires a well-founded evidence. On the Ukrainian Shield, such objects include the Sushchany-Perga deep fault. To substantiate its deep connection with the mantle, fluorite was informative. The results of its research formed the basis of this work.

Keywords: chondrite-rationing, fluorite, ICP-MS analysis, Sushchany-Perga ore zone
  1. Haletskyy, L. S., Naumenko, U. Z. & Cherniyenko, N. M. (2016). The main types of ore-bearing structure of Ukraine. Mineral'ni resursy Ukrayiny, No. 4, pp. 12-19 (in Ukrainian).
  2. Metalidi, S. V. & Nechayev, S. V. (1983). Sushchany-Perga zone. Geology, mineralogy, ore-bearing. Kyiv: Nau kova Dumka (in Russian).
  3. Chumak, D. M. (2006). Fluorite. Mineral deposits of Ukraine. Vol. 2. Industrial mineral deposits (pp. 239-250). Kyiv, Lviv: Tsentr Yevropy (in Ukrainian).
  4. Ponomarenko, O. M., Samchuk, A. I., Krasyuk, O. P., Makarenko, T. I. & Antonenko, O. H. (2008). Analytical Schemes of Microwave Decomposition of Rocks and Minerals and Microelements Determination in Them by Mass-Spectrometry with Induction Connected Plasma Method (ICP-MS). Mineral. J., 30, No. 4, pp. 97-103 (in Ukrainian).
  5. Ponomarenko, O., Samchuk, A., Ohar, T., Petrychenko, K., Popenko, E. & Krasyuk, O. (2012). Definitions of rare earth elements in rocks and minerals by mass spectrometry induction coupled plasma (ICP-MS). Ukrainian geologist, No. 3, pp. 36-40 (in Ukrainian).
  6. McDonough, W. F. & Sun, S. S. (1995). The composition of the Earth II. Chem. geol., 120, pp. 223-253.
  7. Arkhangelska, V. V. (2008). Unique mineral look — rare-earth fluorite with unusually high content of in frequent lands and yttrium. Proceedings of the International mineralogy seminar Structure and variety of the mineral world (pp. 49-50). Syktyvkar: Geoprint (in Russian).
  8. Hurov, E. P. & Hurova, Ye. P. (1974). Fluocerite from metasomatic rocks of Ukrainian shield. Mineral. zb. Lviv. geol. t-va., No. 28, Iss. 4, pp. 41-43 (in Russian).
  9. Hurov, E. P., Hurova, E. P., Lohinova, L. H. & Lavytskyy, Yu. A. (1975). Fluocerite from pegmatites and metasomatit of a northwest part of the Ukrainian shield. Zap. vsesoyuz. mineral. o-va, Pt. 104, Iss. 4, pp. 455-458 (in Russian).
  10. Voznyak, D. K., Ponomarenko, O. M., Samchuk, A. I., Strekozov, S. M., Belskyy, V. M. & Kosorukov, O. O. (2017). Formation specifics of Pokrovo-Kyriyiv fluorspar deposit in Azov Region (Ukrainian Shield). Mineral. j., 39, No. 1, pp. 75-83 (in Ukrainian).