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Vol 183
Pages:
101-111
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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.

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