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Vol 206
Pages:
26-30
Download volume:
RUS
Article
Geology

Composition features of monazite and xenotime as a basis of partition of Verkhneurmiysky granite massif (Amur river region)

Authors:
N. A. Egorova1
V. I. Alekseev2
About authors
  • 1 — student National Mineral Resources University (Mining University)
  • 2 — Ph.D. associate professor National Mineral Resources University (Mining University)
Date submitted:
2013-01-14
Date accepted:
2013-03-16
Date published:
2013-12-27

Abstract

The main lines of monazite-(Ce) and xenotime-(Y) composition evolution were established in granitoids of the Verkhneurmiysky massif in Amur River region. It is suggested to use revealed features of accessory phosphates composition for a regional partition of granitoids and the assessment of intrusive massifs orepotential.

Область исследования:
Geology
Keywords:
monazite xenotime granitoids Amur River region
Go to volume 206

References

  1. Мarin Y.B. Accessory minerals of granitoid series of tin and molybdenic provinces // Proceedings RMO. 2004. N 6. P.1-7.
  2. Semenov Е.I. Orudeneniye and mineralization of rare earths, thorium and uranium (lanthanides and actinides). Мoscow, 2001. 307 p.
  3. McDonough W.F., Sun S.-s. The composition of the Earth // Chem. Geol. 1995. Vol.120. P.223-253.

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