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Vol 183
Pages:
88-94
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New source of noble corundum in Kenya

Authors:
L. V. Kulachkov1
K. Kamwathi2
V. L. Shterhun3
About authors
  • 1 — Ph.D. Assistant Professor Saint-Petersburg State Mining Institute (Technical University)
  • 2 — President of Company Kennedy International Ltd
  • 3 — Geologist of 1st category All-Russian State Research Geological Institute
Date submitted:
2008-10-09
Date accepted:
2008-12-12
Date published:
2009-04-01

Abstract

The large-scale occurrence of ruby and sapphire in Kenya is represented by contemporary river-bed and valley alluvial placers. The first ones are characterized by a high content of ruby (up to 10,4 ct/m 3 ), the second type is interesting due to the amount of forecasted resources: up to 2,3 million ct of ruby and 1,2 million ct of sapphire. It turned out to trace the mechanism of corundum concentrations forming, the mineral crystallized in Archean high-alumina gneisses affected by Precambrian basites (ultrabasites), and then survived a complicated way: – ancient eluvium – ancient alluvium – transportation by basaltic Pleistocenic magma – Holocenic weathering crust of volcanites – talus – contemporary alluvium.

Keywords:
Ruby sapphire Kenya alluvial placer genesis
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References

  1. Киевленко Е.Я. Геология месторождений драгоценных камней / Е.Я.Киевленко, Н.Н.Сенкевич, А.П.Гаврилов. 2-е изд. М.: Недра, 1982. 279 с.
  2. Haghes R.W. Ruby & Sapphire / RWH publishing Boulder. Colorado. USA. 1997. 512 p.
  3. Saggerson Е.P. Geology of the Simba – Kibwezi area / Ministry of Commerce and Industry, geological survey of Kenya. Rep. № 58. 1963. 70 p.
  4. Saurin E. Some gem occurrences in Cambodia // Rocks & Miner. 1957. Vol.32, № 7-8, pp.397-398.

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