Geological Structure of the Novaya Zemlya Archipelago (West Russian Arctic) and Peculiarities of the Tectonics of the Eurasian Arctic

[1] Bolshiyanov D. Yu.(2009)New data on the coastlines of archipelagos Franz Josef Land, Novaya Zemlya, and Spitsbergen Arctic Antarctic Res. 82 68-77

[2] Pogodina I. A.(2008)Geological implications of the thermochemical model of plumes Russ. Geol. Geophys. 49 441-454

[3] Gusev E. A.(2013)Mesozoic–Cenozoic volcanism and geodynamic events in the Central and Eastern Arctic Russ. Geol. Geophys. 54 874-887

[4] Sharin V. V.(2006)Rapid subsidence of the Barents shelf in the last 15 to 16 ka Geotectonics, No. 3 31-42

[5] Alekseev V. V.(2007)Signs of neotectonic activity of the Barents sea shelf Geotectonics, No. 2 63-78

[6] Dymov V. A.(2018)Geological and paleooceanological significance of the psephitic material from the Cretaceous–Cenozoic deposits from the near-pole part of the Lomonosov Ridge Arctic Antarctic Res. 64 182-199

[7] Anokhin V. M.(2008)Tectonotype of volcanic passive margins in the Norwegian–Greenland region Geotectonics 42 225-244

[8] Anikina N. Yu.(1996)“Neotectonics of Arctic continental margins,” Izv Phys. Solid Earth 32 986-991

[9] Derevyanko L. G.(1999)Upper Devonian–Carboniferous ophiolites and bathyal group of the Polar Urals Dokl. Akad. Nauk 365 802-805

[10] Dobretsov N. L.(2017)Duration, causes, and geodynamic significance of the Mid-Cenozoic hiatus in sedimentation at the near-pole part of the Lomonosov Ridge (based on IODP‑302-ACEX data) Oceanology 57 675-584

[1] Bolshiyanov D. Yu.(2009)New data on the coastlines of archipelagos Franz Josef Land, Novaya Zemlya, and Spitsbergen Arctic Antarctic Res. 82 68-77

[2] Pogodina I. A.(2008)Geological implications of the thermochemical model of plumes Russ. Geol. Geophys. 49 441-454

[3] Gusev E. A.(2013)Mesozoic–Cenozoic volcanism and geodynamic events in the Central and Eastern Arctic Russ. Geol. Geophys. 54 874-887

[4] Sharin V. V.(2006)Rapid subsidence of the Barents shelf in the last 15 to 16 ka Geotectonics, No. 3 31-42

[5] Alekseev V. V.(2007)Signs of neotectonic activity of the Barents sea shelf Geotectonics, No. 2 63-78

[6] Dymov V. A.(2018)Geological and paleooceanological significance of the psephitic material from the Cretaceous–Cenozoic deposits from the near-pole part of the Lomonosov Ridge Arctic Antarctic Res. 64 182-199

[7] Anokhin V. M.(2008)Tectonotype of volcanic passive margins in the Norwegian–Greenland region Geotectonics 42 225-244

[8] Anikina N. Yu.(1996)“Neotectonics of Arctic continental margins,” Izv Phys. Solid Earth 32 986-991

[9] Derevyanko L. G.(1999)Upper Devonian–Carboniferous ophiolites and bathyal group of the Polar Urals Dokl. Akad. Nauk 365 802-805

[10] Dobretsov N. L.(2017)Duration, causes, and geodynamic significance of the Mid-Cenozoic hiatus in sedimentation at the near-pole part of the Lomonosov Ridge (based on IODP‑302-ACEX data) Oceanology 57 675-584