Abstract
The pyrite in the high-temperature quartz-gold ore associations and in the root parts of the orebodies is enriched in Mo, Ti, Cr, Co, Ni, V, As, U, and Th; that in the medium-temperature quartz-gold sulphide associations at the middle parts of the bodies has high contents of Au, Cu, Pb, and Zn, while the medium- to low-temperature associations and the upper parts of the orebodies show enrichment in Ag, Sb, Hg. The thermo-emf of pyrite varies regularly in space: along the dip and strike, the proportion of pyrite with electron conductivity increases. These properties that typify the mineral enable us to identify the zoning in deposits, the erosion levels, and the abundances of various types of ore at depth. -from Journal summary
| Original language | English |
|---|---|
| Pages (from-to) | 145-155 |
| Number of pages | 11 |
| Journal | Geochemistry International |
| Volume | 22 |
| Issue number | 5 |
| Publication status | Published - 1985 |
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ASJC Scopus subject areas
- Geochemistry and Petrology
- Geophysics
Cite this
Geochemical features of pyrite in gold-ore deposits. / Korobeynikov, A. F.; Pshenichkin, A. Y.
In: Geochemistry International, Vol. 22, No. 5, 1985, p. 145-155.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Geochemical features of pyrite in gold-ore deposits.
AU - Korobeynikov, A. F.
AU - Pshenichkin, A. Y.
PY - 1985
Y1 - 1985
N2 - The pyrite in the high-temperature quartz-gold ore associations and in the root parts of the orebodies is enriched in Mo, Ti, Cr, Co, Ni, V, As, U, and Th; that in the medium-temperature quartz-gold sulphide associations at the middle parts of the bodies has high contents of Au, Cu, Pb, and Zn, while the medium- to low-temperature associations and the upper parts of the orebodies show enrichment in Ag, Sb, Hg. The thermo-emf of pyrite varies regularly in space: along the dip and strike, the proportion of pyrite with electron conductivity increases. These properties that typify the mineral enable us to identify the zoning in deposits, the erosion levels, and the abundances of various types of ore at depth. -from Journal summary
AB - The pyrite in the high-temperature quartz-gold ore associations and in the root parts of the orebodies is enriched in Mo, Ti, Cr, Co, Ni, V, As, U, and Th; that in the medium-temperature quartz-gold sulphide associations at the middle parts of the bodies has high contents of Au, Cu, Pb, and Zn, while the medium- to low-temperature associations and the upper parts of the orebodies show enrichment in Ag, Sb, Hg. The thermo-emf of pyrite varies regularly in space: along the dip and strike, the proportion of pyrite with electron conductivity increases. These properties that typify the mineral enable us to identify the zoning in deposits, the erosion levels, and the abundances of various types of ore at depth. -from Journal summary
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M3 - Article
AN - SCOPUS:0022265102
VL - 22
SP - 145
EP - 155
JO - Geochemistry International
JF - Geochemistry International
SN - 0016-7029
IS - 5
ER -