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Vol 200
Pages:
114-125
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RUS
Article

Ongonitic magmatism of the Badzhalsky ore district (Amur River region)

Authors:
V. I. Alekseev
About authors
  • Ph.D. associate professor National Mineral Resources University (Mining University)
Date submitted:
2012-07-19
Date accepted:
2012-09-04
Date published:
2013-04-16

Abstract

In the Mesozoic history of the volcano-plutonic magmatism of Badzhalsky area the fourth Late Cretaceous ongonitic stage is specified. The ongonitic magmatism of the Amur River region was evolving during several hundreds of thousand years, had cellular nature and eventuated in the zinnwaldite-microcline-albite granitoids formation with rare-metal accessory complex. In the near-contact zone of the Verhneurmiysky massif Pravourmiysky ongonitic complex, which controls the biggest tungsten-stanniferous deposits of the area and includes ongonite dykes and rare-metal granites of the Dozhdlivy intrusive dome, is determined.

Область исследования:
(Archived) Geology and metallogeny
Keywords:
ongonitic magmatism rare-metal granite ongonite tungsten-stanniferous deposits Badzhalsky area Amur River region
Funding:

None

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References

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  3. Brousnicyn A.I., Panova E.G., Smolensky V.V. Finds of lithium-fluoric geochemical type granites within the bounds of Verhneurmiysky ore cluster // Izvestiya VUZov. Geology and prospecting. 1993. No 6. P.150-153.
  4. Vladimirov A.G., Annikova I.Yu., Antipin V.S. Ongonite -elvanite magmatism of the South Siberia // Litosfera. 2007. No 4. P.21-40.
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  8. Krukov V.G., Sherbak L.I. Geology and metallogeny of the Badzhalsky stanniferous area (Amur River re-gion) // Soviet geology. 1987. 3. P.55-65.
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