Email this article Integral Deep Models of the Pechenga and Onega Ore Regions
- Authors: Sharov N.V.1, Lobanov K.V.2, Chicherov M.V.2
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Affiliations:
- Institute of Geology, Karelian Science Center
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Issue: Vol 482, No 2 (2018)
- Pages: 1302-1305
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/194188
- DOI: https://doi.org/10.1134/S1028334X18100276
- ID: 194188
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Abstract
A new interpretation of the geological and seismic data demonstratd a correlation between the surface structures of endogenic ore regions of the Baltic Shield, the Moho surface relief, and local heterogeneities in the Earth’s crust. As a result, based on consistent analysis of the geological and seismic data, models of the deep structure of the Pechenga and Onega ore regions were constructed and compared.
About the authors
N. V. Sharov
Institute of Geology, Karelian Science Center
Email: chicher@igem.ru
Russian Federation, Petrtozavodsk, 185910
K. V. Lobanov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: chicher@igem.ru
Russian Federation, Moscow, 119017
M. V. Chicherov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Author for correspondence.
Email: chicher@igem.ru
Russian Federation, Moscow, 119017
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