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
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.
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