Other Mafic-Ultramafic Intrusions of the Chiney Intrusive Complex

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


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.


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© 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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