Submit an Article
Become a reviewer
Geology and metallogeny

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

Authors:
V. I. Alekseev
  • National Mineral Resources University (Mining University)
Date submitted:
2016-11-10
Date published:
2013-01-01

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.

Go to volume 200

Similar articles

Complex examination of grounds on the sewage lines by geophysical methods
2013 A. F. Volynin
Georadar researches of structural features and water cutting of overburden rocks for coal open-cast mining
2013 G. A. Kulyandin, A. V. Omel'yanenko, L. L. Fedorova
Hydrocarbon systems of Siberian platform
2013 V. B. Archegov