Submit an Article
Become a reviewer
Vol 224
Pages:
149-155
Download volume:
RUS ENG
Article
Geology

Evolution of mineral forms of rare element accumulation in ore-bearing granites and meta-somatites of Verkhneurmiysk ore cluster (Priamur region)

Authors:
V. I. Alekseev1
K. G. Sukhanova2
I. M. Gembitskayaya3
About authors
  • 1 — Ph.D., Dr.Sci. professor Saint-Petersburg Mining University
  • 2 — engineer Saint-Petersburg Mining University
  • 3 — Ph.D. leading researcher Saint-Petersburg Mining University
Date submitted:
2016-11-03
Date accepted:
2016-12-27
Date published:
2017-04-14

Abstract

It has been attempted to expand existing understanding of accessory mineralization evolution of rare metal-granite series at post-magmatic stage of their development and formation of associated hydrothermal deposits. Composition and distribution of rare elements of Verkhneurmiysk ore cluster have been examined from the position of mineralogy: the study focused on accessory and ore minerals Sn, W, Nb, Ta, Bi, Y, rare earth elements in rare metal Li-F granites and associated metasomatites. It has been discovered that accessory magmatic and hydrothermal mineral complexes share the same geochemical features, are formed under the leading role of abovementioned elements and consistently follow each other over time. It has been traced how mineral forms of accumulation of Sn, W, Nb, Ta, Y and rare earth elements evolve in the processes of magmatic crystallization and post-magmatic metasomatism in the time series: rare metal granites → zwitters → tourmalinites → chloritites. Mineral rocks of each stage were noted to inherit mineralogical and geochemical distinctions from the rocks of the previous stage. A significant number of minerals, forming in the course of two-three stages, have been discovered, as well as omnipresent magmagene-hydrothermal minerals. For a number of accessory minerals of rare metal granites post-magmatic generations have been identified. Special diversity among accessories of rare metal granites and zwitters was observed in tungsten, tin and bismuth minerals.

Область исследования:
Geology
Keywords:
evolution accessory minerals rare metal granites zwitters tourmalinites Verkhneurmiysk ore cluster Priamur region
10.18454/pmi.2017.2.149
Go to volume 224

Funding

Research has been carried out with financial support from Russian Foundation for Basic Research (project No 14-05-00364а) and Ministry of Education and Science of Russian Federation (basic and project parts of the state order in the field of science No 5.9248.2017/VU in 2017-2019)

Similar articles

Chemistry as a basis for solving environmental issues
2017 V. E. Kogan, T. S. Shakhparonova
Result of combining data from impulse electrical prospecting and aeromagnetic prospecting for groundwater exploration in the south of Yakutia
2017 A. Yu. Davydenko, N. A. Aikasheva, S. V. Bukhalov, Yu. A. Davydenko
Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverse
2017 A. N. Shevtsov, A. A. Zhamaletdinov, V. V. Kolobov, M. B. Barannik
Prospects of obtaining samples of bottom sediments from subglacial lake Vostok
2017 N. I. Vasilev, G. L. Leichenkov, E. A. Zagrivnyi
Problems of mineral tax computation in the oil and gas sector
2017 N. G. Privalov, S. G. Privalova
Inversion modeling of the natural state and production history of Mutnovsky geothermal field in 1986-2006
2017 A. V. Kiryukhin, O. O. Usacheva