Results of integrated geological-geophysical work at the sulfide ore occurrence site (Northern Karelia)
Abstract
The ore occurrence is located on the shore of the White Sea. Structurally, it is located within a narrow graben-like synclinal fold, confined to the western limb of the Primorsky anticlinorium and composed of Archean metamorphic rocks: garnet, feldspar and monomineral amphibolites interbedded with biotite-amphibole, biotite and zoisite-biotite-amphibole gneisses.
Область исследования:
(Archived) Without section
Funding:
None
References
- Dakhnov V. N. Electric Exploration of Oil and Gas Fields. M., Gostoptekhizdat, 1953 (in Russian)
- Zakharov V. Kh. Dipole Inductive Profiling with Amplitude-Phase Measurements in Prospecting and Exploration of Sulfide Ores. L., Nedra, 1967 (in Russian)
- Sveshnikov G. B. Electrochemical Processes at Sulfide Deposits. L., Izd-vo LGU, 1967 (in Russian)
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