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Vol 200
Pages:
81
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Conditions of the natural electric field formation at the silicate nickel deposits of weathering crust

Authors:
O. F. Putikov1
V. G. Lazarenkov2
I. V. Talovina3
N. P. Sechina4
About authors
  • 1 — National Mineral Resources University (Mining University)
  • 2 — National Mineral Resources University (Mining University)
  • 3 — National Mineral Resources University (Mining University)
  • 4 — National Mineral Resources University (Mining University)
Date submitted:
2012-07-17
Date accepted:
2012-09-13
Date published:
2013-01-01

Abstract

Possibility of the natural electric field formation in conditions of the lateritic  weathering crust of the ultra basic rocks in presence of extended in depth  magnetite bearing bodies is proved. Theoretical curves of concentration of the dissolved oxygen and oxidized forms of magnetite are obtained. It is enough satisfied coincidence with the experimental data.

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References

  1. Комаров В.А. Геоэлектрохимия. СПб: Изд-во СПбГУ, 1994. 136 с.
  2. Никеленосные оксиды железа Буруктальского месторождения, Южный Урал / С.О.Рыжкова, И.В.Таловина, В.Г.Лазаренков, В.Л.Уголков, Н.И.Воронцова // Записки Горного института. 2009. Т.183. С.101-111.
  3. Путиков О.Ф. Основы теории нелинейных геоэлектрохимических методов поисков и разведки / Санкт-Петербургский горный институт. СПб, 2009. 534 с.
  4. Свешников Г.Б. Электрохимические процессы на сульфидных месторождениях. Л.: Недра, 1967. 158 с.
  5. Электроразведка: Справочник геофизика. М.: Недра, 1979. 518 с.

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