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Vol 196
Pages:
31
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Distribution of rare earth elements in ores Elov and Buructal supergene nickel deposits

Authors:
A. G. Pilyugin1
I. V. Talovina2
N. I. Vorontsova3
S. O. Ryzhkova4
O. P. Mezentseva5
About authors
  • 1 — Saint Petersburg State Mining University
  • 2 — Saint Petersburg State Mining University
  • 3 — Saint Petersburg State Mining University
  • 4 — Saint Petersburg State Mining University
  • 5 — Saint Petersburg State Mining University
Date submitted:
2011-08-18
Date accepted:
2011-10-20
Date published:
2012-02-01

Abstract

Weathering processes and infiltration metasomatic processes in the weathering crusts hyperbasite arrays have a positive effect  on  the accumulation  of rare earth  elements. The content of rare earth elements is steadily increasing bottom-up on the profile of weathering.  Metasomatic upper profile characterized by a high content  of rare earth  elements, which leads to  the appearance of rare earth elements phosphate mineral phase – xenotime found in this laterite for the first time. The composition of the rare earth elements in incorporating their metasomatic and minerals demonstrates chondritic distribution.

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References

  1. Балашов Ю.А. Геохимия редкоземельных элементов. М., 1976.
  2. Вершинин А.С. Геология, поиски и разведка ги- пергенных месторождений никеля. М., 1993.
  3. Никитин К.К. Никеленосные коры выветривания ультрабазитов и методы их изучения. М., 1970.
  4. McDonough W.F. Constrains of the composition of continental litospheric mantle // EPSL. 1990. Vol.101.
  5. № 1. P.1-18.

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