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Geology

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
  • 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:
2016-11-17
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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