Abstract
The distribution of gold, silver, platinum, palladium, and rhodium in the Belozerka and Chara-Tokko greenstone structures is examined. The average Au content in both areas was found to be 10.6-22, which is 2.5-5 times higher than the normal background level (3.1-4.1 ppb). Three types of geochemical anomalies were identified: Au-Ag-As, Pt-Pd-Rh, and Au-Ag-PGE. These anomalies are confined to zones of faulting and hydrothermal metasomatism. Of particular interest are Au-Ag anomalies in fault zones in Archean metaterrigenous rocks and Au-Ag-PGE in magnetite quartzites containing sodic metasojnatites. Further work is required to assay these anomalies for the entire set of noble metals.
| Original language | English |
|---|---|
| Pages (from-to) | 1032-1040 |
| Number of pages | 9 |
| Journal | Geochemistry International |
| Volume | 34 |
| Issue number | 12 |
| Publication status | Published - 1996 |
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ASJC Scopus subject areas
- Geochemistry and Petrology
- Geophysics
Cite this
Geochemical background and anomalies of noble metals in upper archean volcanic-terrigenous formations of greenstone belts in the Aldan and Ukrainian shields. / Korobeinikov, A. F.; Kravchenko, V. M.; Pikarenya, D. S.; Popovchenko, S. E.; Prokopchuk, S. I.
In: Geochemistry International, Vol. 34, No. 12, 1996, p. 1032-1040.Research output: Contribution to journal › Article
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TY - JOUR
T1 - Geochemical background and anomalies of noble metals in upper archean volcanic-terrigenous formations of greenstone belts in the Aldan and Ukrainian shields
AU - Korobeinikov, A. F.
AU - Kravchenko, V. M.
AU - Pikarenya, D. S.
AU - Popovchenko, S. E.
AU - Prokopchuk, S. I.
PY - 1996
Y1 - 1996
N2 - The distribution of gold, silver, platinum, palladium, and rhodium in the Belozerka and Chara-Tokko greenstone structures is examined. The average Au content in both areas was found to be 10.6-22, which is 2.5-5 times higher than the normal background level (3.1-4.1 ppb). Three types of geochemical anomalies were identified: Au-Ag-As, Pt-Pd-Rh, and Au-Ag-PGE. These anomalies are confined to zones of faulting and hydrothermal metasomatism. Of particular interest are Au-Ag anomalies in fault zones in Archean metaterrigenous rocks and Au-Ag-PGE in magnetite quartzites containing sodic metasojnatites. Further work is required to assay these anomalies for the entire set of noble metals.
AB - The distribution of gold, silver, platinum, palladium, and rhodium in the Belozerka and Chara-Tokko greenstone structures is examined. The average Au content in both areas was found to be 10.6-22, which is 2.5-5 times higher than the normal background level (3.1-4.1 ppb). Three types of geochemical anomalies were identified: Au-Ag-As, Pt-Pd-Rh, and Au-Ag-PGE. These anomalies are confined to zones of faulting and hydrothermal metasomatism. Of particular interest are Au-Ag anomalies in fault zones in Archean metaterrigenous rocks and Au-Ag-PGE in magnetite quartzites containing sodic metasojnatites. Further work is required to assay these anomalies for the entire set of noble metals.
UR - http://www.scopus.com/inward/record.url?scp=24644464765&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=24644464765&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:24644464765
VL - 34
SP - 1032
EP - 1040
JO - Geochemistry International
JF - Geochemistry International
SN - 0016-7029
IS - 12
ER -