V.P. Kyrylyuk. PETROPARAGENESES AND POSSIBLE ORIGIN OF THE BUG AREA GRANULITE COMPLEX SUPERCRUSTAL FORMATIONS (WESTERN PART OF UKRAINIAN SHIELD). A r t i c l e 2.  PETROPARAGENESES OF THE SUPERCRUSTAL FORMATIONS AND TYPOMORPHIC FEATURES OF PETROTYPES

Англійська

https://doi.org/10.15407/mineraljournal.41.02.079

UDC 551.71:552.11/.13/.4

V.P. Kyrylyuk, https://orcid.org/0000-0001-7649-9432

M.I. Bogdanova, https://orcid.org/0000-0002-7850-4482

E.I. Savina, https://orcid.org/0000-0001-5551-8630

Ivan Franko National University of Lviv

4, Grushevskogo Str., Lviv, Ukraine, 79005

E-mail: Kyrylyuk.V@i.ua

PETROPARAGENESES AND POSSIBLE ORIGIN OF THE BUG AREA GRANULITE COMPLEX SUPERCRUSTAL FORMATIONS (WESTERN PART OF UKRAINIAN SHIELD).
A r t i c l e 2.  PETROPARAGENESES OF THE SUPERCRUSTAL FORMATIONS AND TYPOMORPHIC FEATURES OF PETROTYPES

Language: Russian

Mineralogical journal 2019, 41 (2): 79-94

Abstract:

Introduction. In the previous article (Mineral. Journ. (Ukraine), Vol. 41, No. 1, pp. 60-70) it was shown that seven main petroparagenses are found in the granulite complex: kinzigite, enderbite-gneiss, leucogranulite, high-aluminous-quartzite, marble-calciphyre, khondalite and aluminous-basite and three minor petroparageneses: calciphyrite-shale, magnetite-containing and metabasite-meta-ultrabasite. Each petroparagenesis includes two to four petrotypes. Composition and typomorphic features of petrotypes. This article describes the characteristic features of petrotypes. The most convenient features used to compare petrotypes are: a) position of rocks in the system SiO2 – (Na2O + K2O); b) the ratio of alkalis; c) M.P. Semenenko’s factors; d) iron and aluminum content, and for some groups of rocks, there are also additional ratios. It is shown that the petroparageneses of the Bug Area complex is distinctly distinguished not only by the sets of its petrotypes, but also by the characteristic features of the composition and structure of the rocks representing them. These features allow us to make an assumption about their initial – volcanogenic or lithogenic – nature of petrotypes. The conclusions are preliminary. They can be refined and extended when considering the origin of petroparageneses in general and the entire initial section of the Bug Area complex in particular. Such general conclusions are given in the 3rd, final article.

Keywords: granulite complex, supercrustal formation, petroparagenesis, petrotype.

References:

  1. Belevtsev, Ya.N., Epatko, Yu.M. and Verigin, M.I. (1981), Precambrian iron-ore deposits of Ukraine and anticipating estimation of them, Nauk. dumka, Kyiv, UA, 232 p.
  2. Bilonizhka, P.M., Gerenchyk, N.K., Zubova, S.N., Kyrylyk, V.P., Lashmanov, V.I. and Martynova, S.S. (1981), Problemy osadochnoy geologii dokembriya, Vyp. 6, Nauka, Moscow, RU, pp. 86-89.
  3. Bogatyryev, V.F., Bystrevskaya, S.S. and Ionis, G.I. (1977), Geol. zhurn., Vol. 37, No. 6, Kyiv, UA, pp. 18-27.
  4. Venidiktov, V.M. (1978), Precambrian of Dniester Area and some geological issues of Ukrainian shield, Nauk. dumka, Kyiv, UA, 162 p.
  5. Vinogradov, G.G. (1970), Petrographiya dokembriya Russkoy platformy, Nauk. dumka, Kyiv, UA, рp. 352-357.
  6. Kyslyuk, V.V., Zyultsle, V.V., Dorkovska, Z.M., Guk, L.V., Bondarenko, V.V., Chernetska, G.Y., Nikitina, L.P. and Kyslyuk, G.V. (2011), Derzhavna geologichna karta Ukrainy, Arkush M-35-XXXVI (Gayvoron), Tsentralnoukrainska seria, 1: 200 000, Kyiv, UA, 115 p.
  7. Dimitrov, G.H. (1977), Charnockitic formation of the Middle Bug Area, Preprint Inst. Geokhimii i Fiziki Mineralov Akad. nauk UkrSSR, Kyiv, UA, 56 p.
  8. Drevin, A.Ya. (1966), Structure, stratigraphy of the Middle Bug Area and prospecting criteria on silicious Nicol, Abstr. dis. cand. geol.-mineral. sci., Kyiv, UA, 23 p.
  9. Drevin, A.Ya. (1967), Problemy osadochnoy geologii dokembriya, Vyp. 2, Nedra, Moscow, RU, pp. 88-96.
  10. Zagnitko, V.N. (1978), Dokl. Akad. Nauk UkrSSR, Ser. B, No. 11, Kyiv, UA, pp. 963-966.
  11. Zagnitko, V.N. and Lugovaya, I.P. (1989), Isotopic geochemistry of carbon-bearing and ferrite rocks of Ukrainian shield, Nauk. dumka, Kyiv, UA, 315 p.
  12. Zlobenko, I.F., Kanevskiy, A.Ya. and Metalidi, S.V. (1983), Sovetskaya geologiya, No. 9, Moscow, RU, pp. 103-108.
  13. Kanevskiy, A.Ya. (1976), Ultrabasic rocks of the Middle Bug Area (formations, petrographical, petrochemical aspects and metal content), Abstr. dis. cand. geol.-mineral. sci., Kyiv, UA, 16 p.
  14. Kanevskiy, A.Ya. and Fomin, A.B. (1973), Sovetskaya geologiya, No. 12, Moscow, RU, рр. 115-124.
  15. Kyrylyuk, V.P. (1982), Geol. zhurn., Vol. 42, No. 3, Kyiv, UA, pp. 88-103.
  16. Kyrylyuk, V.P. (1982), Geol. zhurn., Vol. 42, No. 4, Kyiv, UA, pp. 30-41.
  17. Kyrylyuk, V.P. (2010), Granulitovye strukturno-formatsionnye kompleksy Ukrainskogo schita - evropeyskiy stratotip, ZUKTC press, Lviv, UA, pр. 8-63.
  18. Kyrylyuk, V.P., Bogdanova, M.I. and Savina, E.I. (2019), Mineral. Journ. (Ukraine), Vol. 41, No. 1, Kyiv, UA, pp. 60-70. https://doi.org/10.15407/mineraljournal.41.01.060
  19. Yesypchuk, K.Yu., Bobrov, O.B., Stepanyuk, L.M., Shcherbak, M.P., Glevaskiy, E.B., Skobelev, V.M., Drannik, V.S. and Geichenko, M.V. (2004), Correlated chronostratigraphic scheme of Early Precambrian of the Ukrainian Shield (scheme and explanatory note), NSC Ukraine, UkrDGRI, Kyiv, UA, 30 p.
  20. Lazko, E.M., Kyrylyuk, V.P., Sivoronov, A.A. and Yatsenko, G.M. (1975), Lower Precambrian of the western part of the Ukrainian shield (age complexes and formations), Vyshcha shkola, Lvov, UA, 239 р.
  21. Lesnaya, I.M. and Sobolev, V.B. (2013), Tez. dokl. Mezhdunar. nauch. konf., 27 maia - 1 iyunia 2013, M.P. Semenenko IGMOF of NAS of Ukraine, Kyiv, UA, pp. 86-87.
  22. Andreeva, E.D., Baskina, V.A., Bogatikov, O.E. and et al. (1983), Magmatic rocks. Classification, nomenclature, petrography, Pt 1, Nauka, Moscow, RU, 367 p.
  23. Polovko, N.I., Bondareva, N.M., Kostyuchenko, V.S., Melnichuk, E.V., Bogatyryev, V.F. and Ionis, G.I. (1978), Zhelezisto-kremnistye formatsii Ukrainskogo shchita, Nauk. dymka, Kyiv, UA, pp. 217-253.
  24. Semenenko, N.P. (1966), Metamorphism of the mobile belts, Nauk. dumka, Kyiv, UA, 298 p.
  25. Smirnyiy, V.V. (1968), Materialy po petrografii i geologii mestorozheniy poleznyh iskopaemyh, Tr. VSEGEI, novaya seriya, Vol. 121, Vyp. 1, Leningrad, RU, pp. 179-190.
  26. Sukach, V.S. (1994), Material composition and specific features of genesis of the carbon-bearing rocks of Precambrian of the western part of Ukrainian Shield, Abstr. dis. cand. geol.-mineral. sci., Kyiv, UA, 26 p.
  27. Travin, L.B. (1977), Litologiya i poleznye iskopaemye, No. 3, Moscow, RU, pp. 115-126.
  28. Scherbakov, I.B. (1975), Petrology of Precambrian rocks of the central part of Ukrainian Shield, Nauk. dumka, Kyiv, UA, 279 p.
  29. Yaroshchuk, M.A. (1983), Iron-ore formations of Belaya Tserkov-Odessa metallogenic zones (western part of Ukrainian Shield), Nauk. dumka, Kyiv, UA, 224 p.
  30. Yaroshchuk, M.A., Bogatyryev, V.F. and Epatko, Yu.M. (1982), Geol. zhurn., Vol. 42, No. 3, Kyiv, UA, pp. 48-60.
  31. Yaroshchuk, M.A., Bogatyryev, V.F. and Ionis, G.I. (1981), Metamorphogenic ore formation of the low-temperature facies and ultra metamorphism, Nauka, Moscow, RU, pp. 264-278.
File_attachments: 
PDF icon 2019-2_79-94.pdf