Composition features of monazite and xenotime as a basis of partition of Verkhneurmiysky granite massif (Amur river region)
About authors
- 1 — student National Mineral Resources University (Mining University)
- 2 — Ph.D. associate professor National Mineral Resources University (Mining University)
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
Funding:
None
References
- Мarin Y.B. Accessory minerals of granitoid series of tin and molybdenic provinces // Proceedings RMO. 2004. N 6. P.1-7.
- Semenov Е.I. Orudeneniye and mineralization of rare earths, thorium and uranium (lanthanides and actinides). Мoscow, 2001. 307 p.
- McDonough W.F., Sun S.-s. The composition of the Earth // Chem. Geol. 1995. Vol.120. P.223-253.
Similar articles
Correlation between reactivity, hydrophobicity of surface-modified metal-filler and tribological characteristics of lubricants based on it
2013 A. G. Syrkov, L. A. Yachmenova, E. V. Remzova
Thermodynamics sorption of complex of cerium ions on the anion exchanger
2013 M. A. Ponomareva, O. V. Cheremisina, D. E. Chirkst
Measurement of the seismic blast wave during the construction of the pipeline trench near the existing pipeline
2013 R. A. Vosgrin, L. V. Surovitsky
Estimation of pearameters of stress-and-strain state of rock mass in vicinity of a transport excavation
2013 E. R. Kovalsky, S. P. Mozer, M. A. Medvedskov