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- W2566071856 abstract "The Cenozoic ocean lithosphere transformations in the Arctic Region and their geodynamic nature are studied on the basis of geophysical and geological data. Division into new lithosphere blocks in the Arctic Region at the Cenozoic stage was initiated by the Spitsbergen–Northern Greenland (and its Northern Greenland–Canadian segment) and the Khatanga– Lomonosov transform fault zones. Movement of the Amerasian basin lithosphere block over the faults resulted in the development of fold belts between the continental and oceanic crusts in the southern part of the Canadian basin at the turn of the Oligocene– Miocene. In our opinion, the transformations were caused by deep geodynamics involving the dislocation of mantle bodies by a convection cell towards the Aleutian subduction zone. A major event in evolution of the Cenozoic ocean in the Arctic Region is the formation of the Norwe�" @default.
- W2566071856 created "2017-01-06" @default.
- W2566071856 creator A5042638270 @default.
- W2566071856 date "2012-01-01" @default.
- W2566071856 modified "2023-09-24" @default.
- W2566071856 title "TectonoGeodynamic Transformations of the Amerasian Basin Lithosphere in the Cenozoic E. V. Shipilov a and Corresponding Member of the RAS L. I. Lobkovskii b" @default.
- W2566071856 hasPublicationYear "2012" @default.
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