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
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.
Similar articles
Geophysical data on the structure of the southeastern part of the Wind Belt synclinorium
1974 N. N. Bolgurtsev
Depth of electrical exploration by methods of dipole inductive profiling and ungrounded loop
1974 V. H. Zakharov
On the accuracy of reflecting boundaries in the sections of the Pechenga area
1974 I. V. Litvinenko, A. L. Livantsova, M. D. Lizinsky, M. E. Melamud