Deep Structure of the Pechenga and Onega Ore Districts

Occupation: Research Fellow
Affiliation: Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the RAS
Address: Russian Federation, Moscow

Konstantin Lobanov

Occupation: Chief of IGEM, RAS
Affiliation: Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the RAS
Address: Russian Federation, Moscow

Journal name

Doklady Akademii nauk

Edition

Volume 482 Issue 6

Pages

689-692

Abstract

New interpretation of geological and seismic data has revealed a correlation of surface structures of endogenous ore districts of the Baltic shield Moho topography and local inhomogeneities of the crust. As a result the model of the deep structure of Pechenga and Onega ore districts, based on a agreed analysis of geological and seismic data were constructed and performed their comparison.

Keywords

ore regions, seismic research, Moho discontinuity

Received

07.12.2018

Publication date

13.12.2018

Cite Download pdf To download PDF you should sign in

GOST	Sharov N., Chicherov M., Lobanov K. Deep Structure of the Pechenga and Onega Ore Districts // Doklady Akademii nauk – 2018. – V. 482. – Issue 6 C. 689-692 [Electronic resource]. URL: http://ras.jes.su/dan/s086956520002957-5-1-en (circulation date: 10.10.2024). DOI: 10.31857/S086956520002957-5
MLA	Sharov, Nikolay, Chicherov, Mikhail, Lobanov, Konstantin "Deep Structure of the Pechenga and Onega Ore Districts." Doklady Akademii nauk 482.6 (2018):689-692. DOI: 10.31857/S086956520002957-5
APA	Sharov N., Chicherov M., Lobanov K. (2018). Deep Structure of the Pechenga and Onega Ore Districts. Doklady Akademii nauk 482(6), pp.689-692 DOI: 10.31857/S086956520002957-5

Размещенный ниже текст является ознакомительной версией и может не соответствовать печатной

Readers community rating: votes 0

1. Isanina Eh.V., Verba M.L., Ivanova N.M. Kazanskij V.I., Sharov N.V. Glubinnoe stroenie i sejsmogeologicheskie granitsy Pechengskogo rajona na Baltijskom schite i smezhnoj chasti shel'fovoj plity Barentseva morya // Geologiya rudnykh mestorozhdenij. 2000. T. 42, № 5. S. 476—487.

2. Lobanov K.V. Strukturno-petrofizicheskie usloviya lokalizatsii ranneproterozojskikh pegmatitovykh i magmaticheskikh mestorozhdenij severo-vostochnoj chasti Baltijskogo schita. Avtoreferat dissertatsii na soiskanie uchenoj stepeni doktora geol.-min. nauk. Moskva, IGEM RAN. 2008, 70 s.

3. Onezhskaya paleoproterozojskaya struktura (geologiya, tektonika, glubinnoe stroenie i minerageniya) / otv. red. L.V. Glushanin, N.V. Sharov, V.V. Schiptsov. Petrozavodsk: KarNTs RAN, 2011. 431 s.

4. Sejsmogeologicheskaya model' litosfery Severnoj Evropy: Laplandsko-Pechengskij rajon / otv. red. N.V. Sharov. Apatity: KNTs RAN, 1997. 226 s.

5. Sharov N.V., Isanina Eh.V., Zamozhnyaya N.G., Krupnova N.A., Sulejmanov A.K. // Geofiz. zhurnal. 2011. 33, № 3. S. 23—39.

6. Sharov N.V., Kulikov V.S., Isanina Eh.V, Drogitskaya G.M., Kazanskij V.I. // Geofiz. zhurnal. 2013, № 4 S. 16—28.