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Other Mafic-Ultramafic Intrusions of the Chiney Intrusive Complex

  • Bronislav Gongalsky
  • Nadezhda Krivolutskaya
Chapter
Part of the Modern Approaches in Solid Earth Sciences book series (MASE)

Abstract

The mafic-ultramafic rocks occur on the periphery of the Kodar-Udokan basin. They belong to the Chiney Intrusive Complex. The largest bodies are the Chiney and Luktur plutons, as well as the Upper Sakukan and Mylovskiy layered mafic-ultramafic intrusions. Gabbronorite dikes also belong to the Chiney Complex, with the Main Udokan Dike (up to 200 m thick) being the largest. The geochemical and geophysical data indicate that outcrops of mafic and ultramafic rocks at the margins of the Lurbun granite-granodiorite pluton, which cuts through the Chiney pluton, also belong to the Chiney Complex.

References

  1. Bogatikov OA, Kovalenko VI, Sharkov EV, Yarmoluk VV (2000) Magmatism and geodynamics; terrestrial magmatism throughout the earth’s history. Gordon and Breach Science Publishers, Amsterdam, 511 pGoogle Scholar
  2. Bognibov VI, Krivenko AP, Izokh AE, Tolstykh ND, Glotov AI, Nesterenko GV, Balykin AP, Podlipskiy MJU, Glazunov OM, Mekhonoshin AS, Tsypukov MY, Konnikov EG, Kislov EV, Orsoyev DA, Gongalsky BI, Akhmetov RN, Buchko IV, Datsenko VM (1995) The mafic-ultramafic complexes of south Siberia enriched in platinum. Novosibirsk, Publisher of SIC UIGGM of SB RAS, 151 (in Russian)Google Scholar
  3. Charlier B, Namur O, Latypov R (eds) (2015) Layered intrusions. Springer, Dordrecht, p 762Google Scholar
  4. Dobretsov NL, Konnikov EG, Tsoi LA (1984) A new model for the formation of rhythmic stratification of basic plutons. Geol Geophys 2:3–11 ((in Russian)Google Scholar
  5. Ernst RE (2014) Large igneous provinces. Cambridge University Press, Cambridge, p 666CrossRefGoogle Scholar
  6. Ernst RE, Buchan KL (2004) Large igneous provinces (LIPs) in Canada and adjacent regions: 3 Ga to present. Geosci Can 31–3:103–126Google Scholar
  7. Gongalsky BI (2011) Platinum group metals in rocks and ores of deposits of the Udokan-Chiney region. Platinum Russ VII:253–263 (in Russian)Google Scholar
  8. Gongalsky BI (2015) Deposits of the unique metallogenic province of northern Transbaikalia. Moscow, VIMS 248 (in Russian)Google Scholar
  9. Gongalsky BI, Krivolutskaya NA (1993) The Chiney layered pluton. Nauka, Novosibirsk, p 184 (in Russian)Google Scholar
  10. Gongalsky BI, Krivolutskaya NA (1999) Mineralogy and geochemistry of platinum group metals in the Chiney pluton. Platinum Russ IV:30–40 (in Russian)Google Scholar
  11. Gongalsky BI, Krivolutskaya NA (2004) Noble metal sulfide mineralization in the Chiney pluton. Platinum of Russia V:225–249 (in Russian)Google Scholar
  12. Gongalsky BI, Krivolutskaya NA (2009) The Udokan-Chiney ore-magmatic system. Russ Northwest Geol 42:180–184Google Scholar
  13. Gongalsky BI, Golovatyi AS, Abushkevich SA (1995) Zonal ring structures of the Udokan range. Dokl Akad Nauk 343(1):80–82 (in Russian)Google Scholar
  14. Gongalsky BI, Izokh AE, Krivenko AP, Krivolutskaya NA, Tolstykh ND (2004) Huge concentrations of copper in deposits of the Kodar-Udokan area (northern Transbaikalia). In: Rundkvist DV (ed) Large and superlarge deposits: regularities in formation and emplacement. IGEM, Moscow, pp 206–218 (in Russian)Google Scholar
  15. Gongalsky BI, Krivolutskaya NA, Ariskin AA, Nikolaev GS (2008) Internal structure, composition and genesis of the Chiney anorthosite–gabbronorite pluton, northern Transbaikalia. Geochem Int 46:637–665CrossRefGoogle Scholar
  16. Gongalsky BI, Galyamov AL, Pavlovich GD, Petrov AV, Murashov KY (2015a) A 3D model of the head of a Paleoproterozoic plume in the southern Siberian craton. Large igneous provinces, mantle plumes and Metallogeny in the Earth’s history. Publishing House of VB Sochava/Institute of Geography SB RAS, Irkutsk, pp 45–46 (in Russian)Google Scholar
  17. Hofmann AW (1988) Chemical differentiation of the earth: relationship between mantle, continental crust and oceanic crust. Earth Planet Sci Lett 90:297–314CrossRefGoogle Scholar
  18. Krivolutskaya NA (2016) Siberian traps and Pt-Cu-Ni deposits of the Noril’sk area. Springer, Amsterdam, p 361CrossRefGoogle Scholar
  19. Kruger FJ (2005) Filling the bushveld complex magma chamber: lateral expansion, roof and floor interaction, magmatic unconformities, and the formation of giant chromitite, PGE and T-V-magnetite deposits. Mineral Deposita 40:451–472CrossRefGoogle Scholar
  20. Naldrett AJ (2004) Magmatic sulfide deposits: geology, geochemistry and exploration. Springer, Berlin/New York/Heidelberg, p 727CrossRefGoogle Scholar
  21. Sharkov EV, Smolkin VF, Chistyakov AV, Galkin AS, Kharrasov MK (2002) Geology and metallogeny of the Monchegorsk stratified ore-bearing complex. Russian Arctic: geological history, minerageny, geoecology. VNIIOkeangeologiya, pp 485–494 (in Russian)Google Scholar
  22. Tegner C, Cawthorn RG, Kruger FJ (2006) Cyclicity in the Main and upper zones of the bushveld complex, South Africa: crystallization from a zoned magma sheet. J Petrol 47(11):2257–2279CrossRefGoogle Scholar
  23. Tolstykh ND, Krivenko AP, Krivolutskaya NA, Gongalsky BI, Zhitova LM, Kotel’nikova MV (2004) Mineralization of noble metals of sulfide ores of the Chiney pluton. Platinum Russ V:225–249 (in Russian)Google Scholar
  24. Tombasov IA, Shemelina SF, Afonin GA, Drozdov SA (2004) Governmental geological map of the Russian Federation, scale 1–200000. 2nd edn. Udokan series. O-50-XXXVI (Katugin). Cards. Factory of A.P. Karpinsky Russian Geological Research Institute, St-Petersburg, Russia (in Russian)Google Scholar
  25. Wilson AN (1996) The great dike of Zimbabwe. In: Cawthorn RG (ed) Layered intrusions. Elsevier, Amsterdam, pp 181–230Google Scholar

Copyright information

© Springer Nature Switzerland AG 2019

Authors and Affiliations

  • Bronislav Gongalsky
    • 1
  • Nadezhda Krivolutskaya
    • 2
  1. 1.Institute for Geology of Ore Deposits Petrography, Mineralogy and GeochemistryRussian Academy of SciencesMoscowRussia
  2. 2.Vernadsky Institute of Geochemistry and Analytical ChemistryRussian Academy of SciencesMoscowRussia

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