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Elements Determining in the Geological-Structural Model of the Erdenetuin-Obo Copper-Molybdenum Ore Field, Mongolia

  • M. Zhamsran
  • V. I. Sotnikov
  • A. P. Berzina
  • D. Garamzhav
  • Yu. A. Saryanov
Conference paper
Part of the Special Publication No. 4 of the Society for Geology Applied to Mineral Deposits book series (MINERAL DEPOS., volume 4)

Abstract

Copper-molybdenum mineralization in Mongolia is localized within the limits of regional structures referred to as the superimposed metallogenic belts. The latter is spatially controlled by the late Paleozoic (in Southern Mongolia) and late Paleozoic-early Mesozoic (in Northern Mongolia) volcanic belts, elongate in a sublatitudinal trend. The through-going transverse fault system of the northwest trend has played an important role in forming ore-concentrating structures. Intersection of transverse faults and ones that trend along the volcanic belt account for the development of a block fabric and highly permeable zones that are favourable for the existence of long-lived magmatic centers that host the ore fields.

Keywords

Volcanic Belt Metallogenic Belt Porphyry Dike Porphyry Stock Explosion Breccia 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Geology of the Mongolian People’s Republic, vol II (1973) In: Khasin RA, Borsakovskii YuA, Zonenshain LP (eds) Magmatism, metamorphism, tectonics. Nedra, Moscow, 750 pp (in Russian).Google Scholar
  2. Gretskaya TA, Mossakovsky AA (1969) Some questions of the stratigraphy and structural relation between the Carboniferous and the Triassic in northern Mongolia. Akad Nauk SSSR Izv Ser Geol 2: 56–71 (in Russian)Google Scholar
  3. Khasin RA, Marinov NA, Khurts Ch, Yakimov LI (1977) The Erdenetuin-Obo copper-molybdenum deposit in northern Mongolia. Geol Rudn Mestorozhd 6: 3–15 (in Russian).Google Scholar
  4. Krivtsov AI, Migachev IF, Shishakov VB (1981) Morphogenetic type designs of ore bodies at copper porphyry deposits. Sov Geol 10: 28–41 (in Russian).Google Scholar
  5. Mossakovsky AA, Tomurtagoo O (1976) The Upper Paleozoic of Mongolia. Sovmestnaya Sovetsko- MongoPskaya Geologicheskaya Ekspeditziya, Trudy, vol 15. Nauka, Moscow, 126 pp (in Russian).Google Scholar
  6. Sotnikov VI, Berzina AP, Zhamsran M, Myagmar L (1980) The Tsagan-Suburga molybdenum-copper deposit ( MNP ). Geol Rudn Mestorozhd 3: 34–46 (in Russian).Google Scholar
  7. Yarmolyuk VV, Kovalenko VI (1981) The role of largest faults in the location of continental volcanic rocks of MNR. Akad Nauk SSSR Doklady 256, 2: 436–440 (in Russian)Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 1986

Authors and Affiliations

  • M. Zhamsran
    • 1
  • V. I. Sotnikov
    • 2
  • A. P. Berzina
    • 2
  • D. Garamzhav
    • 1
  • Yu. A. Saryanov
    • 1
  1. 1.Institute of Geology and Mining Industry of the MNUlan BatorMNR
  2. 2.Institute of Geology and GeophysicsSiberian Branch of the USSR Academy of ScienceNovosibirskUSSR

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