24.3 STRATIGRAPHIC LEVELS AND LITHOLOGICAL-GENETIC TYPES OF PALEOPROTEROZOIC METACONGLOMERATES OF KRYVYI RIG BASIN

UDC 551.72: 552.512 (477.63) • 📖 Issue 24/ 2015 • 44-60 pages

 

V.Pokalyuk

V.Pokalyuk Ph.D. (Geol.), Senior Research Fellow, State Institution ―Institute of Environmental Geochemistry of National Academy of Sciences of Ukraine‖, Kyiv, Ukraine, pvskan@ukr.net

Abstract

TThere are three main stratigraphic levels of paleoproterozoic metaconglomerates of Kryvyі Rіg synklinorium of the Ukrainian shield. Provided is information on the lithological-genetic types of metaconglomerates, occurring at different stratigraphic levels of Paleoproterozoic of Kryvyi Rig synclinorium. Metaconglomerates belong to different lithological-genetic types (proluvial-deluvial, alluvial, clastic-beach). They are characterized by individual lithologic-petrographic features, which reflect the tectonic and paleogeographic characteristics of sedimentation and can serve as a fairly reliable correlative types of rocks. The specific character of metaconglomerates of each stratigraphic level is presented by physical, sedimentological, structural and metallogenic criteria. The lower stratigraphic levels of metaconglomerates of Paleoproterozoic of Kryvyi Rig synclinorium (skelevatskaya and gdantsevskaya suites) are similar by the major geological features to following metaconglomerate systems: Witwatersrand (South Africa), Blind river (Canada), Tarkwa (Ghana) and can be attributed to the common type of Precambrian metalliferous metaconglomerates.

 

Key words: Precambrian, Paleoproterozoic, metaconglomerate, metapsefite, Kryvyi Rig basin, Ukrainian shield.

 

Article



Reference

  1. Bordunov, I.N. (1964), Geologiya Kremenchugskogo zhelezorudnogo rajona , Nauk. dumka, Kyiv, UA, 217 p.
  2. Paranko, I., Kurylo, M., Bondar, Y. (2013), Kompleksna ocinka geologichnyh pam’jatok pryrody na prykladi geologichnyh ob’jektiv Kryvorizhzhja, Ukrainian Geologist. No.1, pp. 63–71.
  3. Pokalyuk, V.V., Kulish, E.A. (2004), Geologiya i litogenez dosaksaganskih metamorficheskih kompleksov Krivorozhskogo zhelezorudnogo bassejna, Logos, Kyiv, UA,245 p.
  4. Grechishnikov,  M.P., Grechishnikova, Z.M. (1966), Doslid rekonstrukcii’ dokembrijs’koi’ fizyko-geografichnoi’ obstanovky na osnovi vyvchennja porid nyzhn’oi’ svity kryvoriz’koi, Geol. Journ. Vol. 26. Issue. 2, pp. 3–17.
  5. Kalyaev, G.I. (1965), Tektonika dokembriya Ukrainskoj zhelezorudnoj provincii. Kyiv, UA, 190 p.
  6. Kulish, E.A., Pokalyuk, V.V. (2007), Paleotektonicheskij analiz metaosadochnyh kompleksov rannego dokembriya na primere nizhnej svity Krivbassa, Geol. journal. No. 1, pp. 32–44.
  7. Paranko, I.S., Slivko, Ye.M., Malyuk, B.I. (1992), Geologiya i perspektivy zolotonosnosti nizhnej chasti razreza Krivorozhskoj struktury, Geology and Geochemistry of combustible minerals. No.3, pp. 67–77.
  8. Strygin O.I., Loginov, D.F. (1960), Stratygrafija arkozovogo goryzontu nyzhnoi svity kryvorizkoi serii porid v pivnichnij chastyni Saksaganskogo rajonu, Geol. Journe. Vol. 20, No.1, pp. 81–84.
  9. Yatsenko, G.M., Paranko I.S. (1986), O formaciyah i stratigraficheskom polozhenii metamorfizovannyh terrigennyh tolshch yuzhnoj chasti Osnovnoj sinklinali Krivbassa. Geol. Journe. Vol. 46, No. 4, pp. 118–126.
  10. Paranko, I., Ryabenko, V. (1990), Konglomeraty v formaciyah Ukrainskogo shchita. Inst. of geological Sciences, Academy of Sciences of USSR, Kyiv, 55 p.
  11. Kuleshov M.P. (1957), Vozrastnye vzaimootnosheniya porod Krivorozhskogo rajona, Geol. structure and iron ore of Krivoy Rog basin, Moscow, Gosgeoltechizdat, pp. 24–41.
  12. Rozhkov, I.S. (1969),  Sostoyanie problemy izucheniya zolotonosnosti konglomeratov na territorii SSSR, Nauka, Moscow, pp. 7–28.
  13. Deryabin, N. (1995),  O proiskhozhdenii porod skelevatskoj svity Krivbassa, Geol. Journ. No.2, pp. 110–113.
  14. Paranko, I.S., Mighnickaya, T. P. (1991), Etapy geologicheskogo razvitiya i stratigrafiya Krivorozhskoj struktury, Preprint Academy of Sciences of Ukraine, Inst. of geological Sciences, Kyiv, UA, 51 p.
  15. Goroshnikov, B.I. (1956), Novye dannye o sostave porod v okatannyh obrazovaniyah arkozovogo gorizonta Krivogo Roga, Reports of Sciences Academy of USSR. Vol. 107. No.6, pp. 875–877.
  16. Hodus, L.Y. (1948), Novye mineraly v gal’kah konglomeratov nizhnego otdela Krivorozhskoj svity ,  Scient. notes. Dnepr. state University . VolumeXXXI. Pp. 27–32.
  17. Prozhogin, L.G. (1976a), Novye dannye o vzaimootnosheniyah verhnej i srednej svit Krivorozhskoj serii v Saksaganskom rajone, Geol. journ. Vol. 36. No.3, pp. 75–87.
  18. Prozhogin, L.G.  (1976b), Usloviya rudoobrazovaniya v nizah verhnej svity Saksaganskogo rajona Krivorozhskogo bassena po litologicheskim i paleogeograficheskim dannym, Abstract. Dis. Cand. Sci. (Geol.), Kiev, UA.
  19. Prozhogin, L.G., Gorbatenko, V.G. (1975). Zhelezistye konglomeraty osnovaniya verhnej svity (K 1) v Saksaganskom rajone Krivbassa, Lithology and mineral resources, No.1, pp. 30–38.
  20. Esipchuk, K.Y., Bobrov O.B., Stepanyuk L.M. (2004), Koreljacijna hronostratygrafichna shema rann’ogo dokembriju Ukrai’ns’kogo shhyta, Kiev, UA, 30 p.
  21. Nicolsky A.P. (1967), Stratigraficheskie kompleksy dokembriya Yugo-Zapadnoj chasti Russkoj platformy i zadachi ih kartirovaniya v usloviyah zony ul’trametamorfizma, Problems of the sedimentary geology of the Precambrian. Issue.2, Nedra, Moscow, RU, pp. 32–46.
  22. Nicolsky, A.P., Efimov, A.N. (1960), Geologo-metallogenicheskij ocherk vostochnoj chasti Ukrainskogo shchita. Works of inst. VSEGEI, New Ser. Vol. 37, 162 p.
  23. Paranko, I.S., Yatsenko, G.M. (1990), Metakonglomeratovaya i metapeschanikovo-slancevaya formacii verhnej chasti razreza Krivorozhskoj struktury (gleevatskaya svita). Stat’ya 2. Osobennosti proiskhozhdeniya formacij, Geol. Journe. No. 5, pp.124–130.
  24. Yatsenko, G.M., Paranko, I.S. (1990), Metakonglomeratovaya i metapeschanikovo-slancevaya formacii verhnej chasti razreza Krivorozhskoj struktury (gleevatskaya svita). St.1. Stroenie i sostav, Geol. Journal. No. 4, pp. 86–95.
  25. Mighnickaya, T.P. (1993), Metaosadochnye porody graben-sinklinalej Ukrainskogo shchita, Nauk. Dumka, Kiev, UA, 110 p.
  26. Kulish, E., Pokalyuk, V., Kurlov, N., Mechnikov, Yu. (2010), Gleevatskie metakonglomeraty Krivbassa – kontinental’nye molassy ili melkovodno-bassejnovye otlozheniya?, Geochemistry and ecology. Proceedings of the Institute of environmental Geochemistry, Issue.18. Kyiv,UA, pp. 7–26.
  27. Gavrilenko, V.N. (1993), Metallonosnost’ metaterrigennyh porod skelevatskoj svity krivorozhskoj serii, Kiev, UA, pp. 239–246.
  28. Grechishnikov M.P., Sahatsky I.I. (1973), Do pytannja pro umovy nagromadzhennja zolota u konglomeratah Kryvogo Rogu, Geol. Journ . No.3. Vol.33, pp. 107–111.
  29. Pisemsky, G.V., Ganja, L.M., Bolotova, N.Y. (1969), Predvaritelnye rezultaty izucheniya zolotonosnosti dokembrijskih konglomeratov v rajonah Krivogo Roga i Kurskoj magnitnoj anomalii, Problem metallogenetic ancient conglomerates on the territory of the USSR, Nauka, Moscow, RU, pp. 101–112.
  30. Shirynbekov, N.K. (1976), Sootnoshenie serebra i zolota v konglomeratah i ego geohimicheskoe znachenie , Geochemistry and ore formation. Issue. 5, pp. 92–96.
  31. Velikanov, Y.F. (2011), Ocenka perspektiv rudonosnosti geologicheskih formacij Krivbassa na blagorodnye metally, Scientific basis of geological-economic evaluation of mineral resources of Ukraine and the world , Mater. research Intern. Conference, Kiev, UA, pp.12–13.
  32. Chernyshov, N.M., Nenahov, V.M. (2010), Glavnejshie tipy geodinamicheskih i mineragenicheskih ryadov v obshchej modeli formirovaniya dokembrijskoj litosfery (na primere VKM), Herald of the Voronezh state University, Series: Geology, No. 2, pp. 47–58.
  33. Pokalyuk, V.V.,  Sukach, V.V. (2014), Sedimentogenez v rannem dokembrii Krivorozhskogo zhelezorudnogo bassejna: Litohimicheskie tipy i MINLITH-normativnyj sostav metaosadkov, Scientific Bulletin of national mining University. No. 6, pp. 5–14.