Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics
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...
| Published in: | Geodynamics & Tectonophysics |
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| Main Authors: | , , , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | Russian |
| Published: |
Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch
2017
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| Subjects: | |
| Online Access: | https://www.gt-crust.ru/jour/article/view/331 https://doi.org/10.5800/GT-2017-8-1-0231 |
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Geodynamics & Tectonophysics (E-Journal) |
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Russian |
| topic |
сейсмический профиль 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 Евразийский бассейн Северо-Чукотский бассейн бассейн моря Лаптевых бассейн Восточно-Сибирского моря бассейн Подводников хребет Ломоносова хребет Менделеева хребет Гаккеля бассейн Макарова рифт осадочный бассейн |
| spellingShingle |
сейсмический профиль 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 Евразийский бассейн Северо-Чукотский бассейн бассейн моря Лаптевых бассейн Восточно-Сибирского моря бассейн Подводников хребет Ломоносова хребет Менделеева хребет Гаккеля бассейн Макарова рифт осадочный бассейн A. M. Nikishin E. I. Petrov N. A. Malyshev V. P. Ershova А. М. Никишин Е. И. Петров Н. А. Малышев В. П. Ершова Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics |
| topic_facet |
сейсмический профиль 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 Евразийский бассейн Северо-Чукотский бассейн бассейн моря Лаптевых бассейн Восточно-Сибирского моря бассейн Подводников хребет Ломоносова хребет Менделеева хребет Гаккеля бассейн Макарова рифт осадочный бассейн |
| description |
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. На основе российских сейсмических профилей, полученных в ... |
| format |
Article in Journal/Newspaper |
| author |
A. M. Nikishin E. I. Petrov N. A. Malyshev V. P. Ershova А. М. Никишин Е. И. Петров Н. А. Малышев В. П. Ершова |
| author_facet |
A. M. Nikishin E. I. Petrov N. A. Malyshev V. P. Ershova А. М. Никишин Е. И. Петров Н. А. Малышев В. П. Ершова |
| author_sort |
A. M. Nikishin |
| title |
Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics |
| title_short |
Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics |
| title_full |
Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics |
| title_fullStr |
Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics |
| title_full_unstemmed |
Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics |
| title_sort |
rift systems of the russian eastern arctic shelf and arctic deep water basins: link between geological history and geodynamics |
| publisher |
Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch |
| publishDate |
2017 |
| url |
https://www.gt-crust.ru/jour/article/view/331 https://doi.org/10.5800/GT-2017-8-1-0231 |
| long_lat |
ENVELOPE(166.000,166.000,74.000,74.000) ENVELOPE(90.000,90.000,87.000,87.000) ENVELOPE(170.000,170.000,87.000,87.000) ENVELOPE(133.400,133.400,67.544,67.544) ENVELOPE(80.000,80.000,87.000,87.000) ENVELOPE(153.000,153.000,76.500,76.500) ENVELOPE(-93.035,-93.035,56.912,56.912) ENVELOPE(168.000,168.000,80.500,80.500) |
| geographic |
Arctic Arctic Ocean Laptev Sea Canada East Siberian Sea Gakkel Ridge Makarov Basin Verkhoyansk Eurasia Basin De Long Islands Long Islands Podvodnikov Basin |
| geographic_facet |
Arctic Arctic Ocean Laptev Sea Canada East Siberian Sea Gakkel Ridge Makarov Basin Verkhoyansk Eurasia Basin De Long Islands Long Islands Podvodnikov Basin |
| genre |
Arctic Arctic Arctic Ocean canada basin Chukchi Chukotka De Long Islands East Siberian Sea laptev Laptev Sea Lomonosov Ridge makarov basin |
| genre_facet |
Arctic Arctic Arctic Ocean canada basin Chukchi Chukotka De Long Islands East Siberian Sea laptev Laptev Sea Lomonosov Ridge makarov basin |
| op_source |
Geodynamics & Tectonophysics; Том 8, № 1 (2017); 11-43 Геодинамика и тектонофизика; Том 8, № 1 (2017); 11-43 2078-502X |
| op_relation |
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ftjgat:oai:oai.gtcrust.elpub.ru:article/331 2023-05-15T14:25:10+02:00 Rift systems of the Russian Eastern Arctic shelf and Arctic deep water basins: link between geological history and geodynamics Рифтовые системы шельфа Российской Восточной Арктики и арктического глубоководного бассейна: связь геологической истории и геодинамики A. M. Nikishin E. I. Petrov N. A. Malyshev V. P. Ershova А. М. Никишин Е. И. Петров Н. А. Малышев В. П. Ершова 2017-03-23 application/pdf https://www.gt-crust.ru/jour/article/view/331 https://doi.org/10.5800/GT-2017-8-1-0231 rus rus Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch https://www.gt-crust.ru/jour/article/view/331/247 Akinin V.V., 2012. Late Mesozoic and Cenozoic Magmatism and Lower Crust Modifications in the Northern Framing of Pacific. Doctor of Sci. dissertation. IGEM RAS, Moscow, 320 p. (in Russian) [Акинин В.В. 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CC-BY Geodynamics & Tectonophysics; Том 8, № 1 (2017); 11-43 Геодинамика и тектонофизика; Том 8, № 1 (2017); 11-43 2078-502X сейсмический профиль 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 Евразийский бассейн Северо-Чукотский бассейн бассейн моря Лаптевых бассейн Восточно-Сибирского моря бассейн Подводников хребет Ломоносова хребет Менделеева хребет Гаккеля бассейн Макарова рифт осадочный бассейн info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftjgat https://doi.org/10.5800/GT-2017-8-1-0231 https://doi.org/10.1016/j.epsl.2008.07.036 https://doi.org/10.1029/2007PA001476 https://doi.org/10.1007/s11001-010-9094-9 https://doi.org/10.1016/j.tecto.2011.10.015 https://doi.org/10.1016/j.tecto.2016.0 2022-07-19T15:36:33Z 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. На основе российских сейсмических профилей, полученных в ... Article in Journal/Newspaper Arctic Arctic Arctic Ocean canada basin Chukchi Chukotka De Long Islands East Siberian Sea laptev Laptev Sea Lomonosov Ridge makarov basin Geodynamics & Tectonophysics (E-Journal) Arctic Arctic Ocean Laptev Sea Canada East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) Gakkel Ridge ENVELOPE(90.000,90.000,87.000,87.000) Makarov Basin ENVELOPE(170.000,170.000,87.000,87.000) Verkhoyansk ENVELOPE(133.400,133.400,67.544,67.544) Eurasia Basin ENVELOPE(80.000,80.000,87.000,87.000) De Long Islands ENVELOPE(153.000,153.000,76.500,76.500) Long Islands ENVELOPE(-93.035,-93.035,56.912,56.912) Podvodnikov Basin ENVELOPE(168.000,168.000,80.500,80.500) Geodynamics & Tectonophysics 8 1 11 43 |