Чтение онлайн

Пущаровский Ю.М. Тектоника Северного Ледовитого океана. Геотектоника, 1976, № 2, с. 3–14.

Пущаровский Ю.М. Тектоническая типизация океанских глубоководных впадин. // Фундаментальные проблемы геотектоники. Материалы XL Тектонического совещания. Т. 2. Москва, ГЕОС, 2007, с. 121–122.

Старосельцев В. С. Трансрегиональные линеаменты и движения плит // Разведка и охрана недр, 2007, № 8, с. 15–20

Хаин В.Е. Тектоника континентов и океанов (год 2000) – М.: Научный мир, 2001, с. 511–522.

Backman J., Moran K., McInroy D.B. et al. Sites M0001 – M0004. Expedition 302 Scientists. // Proceedings of the Integrated Ocean Drilling Program. 2006. V. 302, p. 1–115.

Franke D., Hinz K., Oncken O. The Laptev Sea rift // Marine and Petroleum Geology, 2001, No. 18, p. 1083–1127.

Grantz A., Pease V.L., Willard D.A., Phillips R., Clark D. Bedrock cores from 89° North: Implication fo the geologic framework and Neogene paleoceanolograhy of Lomonosov Ridge and a tie to the Barents shelf. // Geol. Soc. Amer. Bull., 2001, v. 113, № 10, pp. 1272–1281.

Grantz A., Clark D., Phillips R. et al. Fanerozoic stratigraphy of Northwind ridge, magnetic anomalies in the Canada basin and the geometry and timing of rifting in the Amerasian basin, Arctic ocean. // Geol. Soc. Amer. Bull. 1998. V. 110,N6, p. 801–820.

Nafe J.B., Drake C.L. Variation with depth in shallow and deep water marine sediments of porosity, density and the velocities of compressional and shear waves // Geophysics, 1967, 22 p. 523–552.

Smith & Wessel, 1990. Smith W.H.F., Wessel P. Gridding with continuous curvature spline in tension // Geophysics. 1990. V.55. No. 3, P. 293–305.

Abstract

During the «Arctic-2007» expedition in Arctic Ocean Rosnedra-VNIIOkeangeologia carried out the geologic-geophysical researches to resolve the problem of geological maintenance of the Russian Federation geopolitical objective on the basis of position specification of outer limit of the continental shelf of the Russian Federation in this region, in particular around the Lomonosov Ridge and in a zone of its transition to adjoining shelf. On the basis of obtained data and according with the earlier researches geodynamic model of this region has been created. This model supports the outer limit of the continental shelf of the Russian Federation declaration in Arctic Ocean. Analysis of the geologic-geophysical data along the «Arctic-2007» section as well as geodynamic model allowed to make a number of new essential conclusions about evolution of Arctic ocean. The area of the Central-Arctic submarine elevations and the East Arctic shelf of Russia are the uniform ensemble of geological structures with the general geological history and synoceanic structural-material transformations of the continental crust.