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Vol 206
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Composition features of monazite and xenotime as a basis of partition of Verkhneurmiysky granite massif (Amur river region)

N. A. Egorova1
V. I. Alekseev2
About authors
  • 1 — National Mineral Resources University (Mining University)
  • 2 — National Mineral Resources University (Mining University)
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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.

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  1. Марин Ю.Б. Акцессорные минералы гранитоидных серий оловянных и молибденовых провинций // Записки РМО. 2004. № 6. С.1-7.
  2. Семенов Е.И. Оруденение и минерализация редких земель, тория и урана (лантанидов и актинитов). М., 2001. 307 с.
  3. McDonough W.F. The composition of the Earth W.F.McDonough, S.-s.Sun // Chem. Geol. 1995. Vol.120. P.223-253.

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