Results of complex geologic-geophysical works at the sulfide ore occurrence site (North 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 wing 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. Moscow, Gostoptekhizdat, 1953,
- Zakharov V. H. Dipole Inductive Profiling with Amplitude-Phase Measurements in Prospecting and Exploration of Sulfide Ores. L., Nedra, 1967.
- Sveshnikov G. B. Electrochemical Processes at Sulfide Deposits. L., PH of LSU, 1967.
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