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

N. A. Egorova; V. I. Alekseev

Vol 206

Pages:

26

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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 — National Mineral Resources University (Mining University)
2 — National Mineral Resources University (Mining University)

Date submitted:

2013-01-14

Date accepted:

2013-03-16

Date published:

2013-07-01

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.

References

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

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

Abstract

References

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