Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics

• Published in: Geodynamics & Tectonophysics
• Main Authors: A. M. Nikishin, E. I. Petrov, N. A. Malyshev, V. P. Ershova
• Format: Article in Journal/Newspaper
• Language: English; Russian
• Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2017
• Subjects: arctic; eurasia basin; north chukchi basin; laptev sea basin; east siberian sea basin; podvodnikov basin; lomonosov ridge; mendeleev ridge; gakkel ridge; makarov basin; rift; sedimentary basin; seismic line; Science; Q; Arctic; Arctic Ocean; Laptev Sea; Canada; East Siberian Sea; Gakkel Ridge; Makarov Basin; Verkhoyansk; Eurasia Basin; De Long Islands; Long Islands; Podvodnikov Basin; canada basin; Chukchi; Chukotka; laptev; Lomonosov Ridge
• Online Access: https://doi.org/10.5800/GT-2017-8-1-0231; https://doaj.org/article/f6fbae008c9949ada6f9238ba2535eb1

In our study, we have developed a new tectonic scheme of the Arctic Ocean, which is based mainly on seismic profiles obtained in the Arctic-2011, Arctic-2012 and Arctic-2014 Projects implemented in Russia. Having interpreted many seismic profiles, we propose a new seismic stratigraphy of the Arctic Ocean. Our main conclusions are drawn from the interpretation of the seismic profiles and the analysis of the regional geological data. The results of our study show that rift systems within the Laptev, the East Siberian and the Chukchi Seas were formed not earlier than Aptian. The geological structure of the Eurasian, Podvodnikov, Toll and Makarov Basins is described in this paper. Having synthesized all the available data on the study area, we propose the following model of the geological history of the Arctic Ocean: 1. The Canada Basin formed till the Aptian (probably, during Hauterivian-Barremian time). 2. During the Aptian-Albian, large-scale tectonic and magmatic events took place, including plume magmatism in the area of the De Long Islands, Mendeleev Ridge and other regions. Continental rifting started after the completion of the Verkhoyansk-Chukotka orogenу, and rifting occurred on the shelf of the Laptev, East Siberian, North Chukchi and South Chukchi basins, and the Chukchi Plateau; simultaneously, continental rifting started in the Podvodnikov and Toll basins. 3. Perhaps the Late Cretaceous rifting continued in the Podvodnikov and Toll basins. 4. At the end of the Late Cretaceous and Paleocene, the Makarov basin was formed by rifting, although local spreading of oceanic crust during its formation cannot be excluded. 5. The Eurasian Basin started to open in the Early Eocene. We, of course, accept that our model of the geological history of the Arctic Ocean, being preliminary and debatable, may need further refining. In this paper, we have shown a link between the continental rift systems on the shelf and the formation history of the Arctic Ocean.