Submit an Article
Become a reviewer
Vol 183
Pages:
101-111
Download volume:
RUS
Article

Nickel-containing iron oxides in the Buruktal deposit, South Urals

Authors:
S. O. Ryzkova1
I. V. Talovina2
V. G. Lazarenkov3
N. I. Vorontsova4
V. L. Ugolkov5
About authors
  • 1 — Post-graduate student, Scientific Secretary Saint-Petersburg State Mining Institute (Technical University)
  • 2 — Ph.D. Assistant Saint-Petersburg State Mining Institute (Technical University)
  • 3 — Ph.D., Dr.Sci. Professor Saint-Petersburg State Mining Institute (Technical University)
  • 4 — Ph.D. Assistant Saint-Petersburg State Mining Institute (Technical University)
  • 5 — Ph.D. Institute of Silicate Chemistry of RAS
Date submitted:
2008-10-01
Date accepted:
2008-12-05
Date published:
2009-12-11

Abstract

In the Buruktal supergene nickel deposit, iron oxides possess vertical mineralogical zoning (bottom-up): magnetite-maghemite-goethite-hematite. The main rock- and ore-forming mineral in the iron-oxide zone of the deposit is magnetite, presented by three generations: primary relic magnetite, surviving from ultramafic rocks; secondary magnetite, forming at serpentinization process and neogenic supergene magnetite. Supergene magnetite, like a goethite, is nickel ore mineral, containing about 1 % NiO. Under the complex thermal analysis data, maghemite-magnetite and goethite have two main diagnostic maximums: exothermal effect of magnetite, caused by magnetite oxidation to maghemite in the interval 317‑340 °С, displays maximum at 327 °С («magnetite» point), and endothermic effect of goethite, connected with loss of constitutional water of the mineral and its transition to hematite in the interval 269‑296 °С, displays maximum at 288 °С («goethite» point).

Область исследования:
(Archived) Geology, search and prospecting of mineral deposits
Keywords:
weathering crust iron-oxide zone serpentinites magnetite
Go to volume 183

References

  1. Varlakov A.S. Petrology of serpentinization process in hyperbasites of folded regions. Sverdlovsk: Publ. UNZ AS USSR, 1986. 24 p.
  2. Deer W.А. Rock-forming minerals / W.А.Deer, R.А.Howie, J.Zussman. М.: Mir, 1966. Vol.3. 316 p.
  3. Kapustkin G.R. Mineralogical features in iron oxide-hydroxide forming during weathering of serpentinites in South Urals / G.R.Kapustkin, I.E.Gorshkova, A.V.Savtsov // Weathering crust. М.: Nauka, 1986. Vol.19, pp. 66-77.
  4. Kuzemkina Е.N. Nickel containing magnetite. // In: «Nickel weathering crusts in Urals». М.: Nauka, 1970, pp.193-202.
  5. Edelshtein I.I. Substantial content of weathering product on ultramafic rocks in Buruktal massif // Materials to geology and mineral resources in South Urals. M.: Gosgeoltechizdat, 1956. Vol.1, pp. 38-60.
  6. Incorporation of Ni into natural goethite: An investigation by X-ray absorption spectroscopy / M.L.Carvalho-e-Silva, A.Y.Ramos, A.C.N.Tolentino, J.Enzweiler, S.M.Netto, M.C.M.Alves // Amer. Mineral., 2003. Vol.88, pp.876-882.
  7. Manceau A. Heterogeneous distribution of nickel in hidrous silicates from New Caledonia ore deposits /
  8. A.Manceau, G.Calas // Amer. Mineral., 2000. Vol.0, pp.9-558.
  9. Shellmann W. Behaviour of nickel, cobalt and cromium in ferrigionous lateritic nickel ores // Bull. BRGM, 1978. Ser II. № 3ю Sec.II. pp.275-282.

Similar articles

On specific features of stratigraphy of the middle devonian deposits of the Leningrad region
2009 M. G. Tsinkoburova
New source of noble corundum in Kenya
2009 L. V. Kulachkov, K. Kamwathi, V. L. Shterhun
Composition of retrospective geological systems and significance of structural-tectonic factor in paleogeographic reconstructions
2009 V. P. Matveev
Regularities of changes in strength of rocks under complicated stress state, different levels of humidity and pore pressure
2009 A. T. Karmansky
Results of profile magnetotelluric researches at the Ozernoye ore cluster in Buryatiya Republic
2009 M. M. Pechenkin, A. N. Shelekhov, L. I. Bogatyrev
New data on infrared spectroscopy of diamonds from industrial deposits of Yakutia
2009 I. N. Bogush, S. I. Mityukhin, E. A. Vasiliev