2007
DOI: 10.1134/s0016852107030016
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Tectonics of the eastern Arctic region

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Cited by 25 publications
(9 citation statements)
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“…Burlin & Stoupakova (2008). Modified from Bogdanov & Khain (1996a, b), Milanovskiy (1987Milanovskiy ( , 1991, Gabrielsen et al (1990), Johansen (1994), Suprunenko et al (2004) and Filatova & Khain (2007). 1, Stable platform areas; 2, intracratonic rift systems with inherited extensional depressions and inverted swells; 3, inverted swells; 4, sag basins, overlying older structures; 5, domes and uplifts; 6, Baikalian folding; 7, Caledonian folding; 8, Hercynian folding; 9, Cimmerian folding: a, more dislocated; b, less dislocated; b, poorly dislocated; 10, volcanic belts; 11, oceanic rifting; 12, deep faults; 13, continental slope margin; 14, coast line.…”
Section: Intracratonic Riftingmentioning
confidence: 95%
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“…Burlin & Stoupakova (2008). Modified from Bogdanov & Khain (1996a, b), Milanovskiy (1987Milanovskiy ( , 1991, Gabrielsen et al (1990), Johansen (1994), Suprunenko et al (2004) and Filatova & Khain (2007). 1, Stable platform areas; 2, intracratonic rift systems with inherited extensional depressions and inverted swells; 3, inverted swells; 4, sag basins, overlying older structures; 5, domes and uplifts; 6, Baikalian folding; 7, Caledonian folding; 8, Hercynian folding; 9, Cimmerian folding: a, more dislocated; b, less dislocated; b, poorly dislocated; 10, volcanic belts; 11, oceanic rifting; 12, deep faults; 13, continental slope margin; 14, coast line.…”
Section: Intracratonic Riftingmentioning
confidence: 95%
“…There are some large residual cratonic and volcanic massifs with individual relics of Palaeozoic rifts and grabens traced within the Chukchi Sea, the East Siberia Sea and the Laptev Sea. Upper Palaeozoic -Lower Mesozoic terrigenouscarbonate complexes are at the surface within adjacent linear inverted swells, fold and thrust belts, such as the WrangelHerald range and the Verkhoyansk fold belt (Sekretov 2002;Burlin & Shipelkevich 2006;Filatova & Khain 2007).…”
Section: Eurasian and Amerasian Basinsmentioning
confidence: 99%
“…The origin of Vilkitskii Basin is uncertain but the limited observations of structural and stratigraphic features and its regional setting are generally compatible with an early episode (Jurassic-Cretaceous) of crustal extension related to opening of the Amerasia Basin coincident with the Brooks Range-Chukotka orogeny and northward sediment dispersal followed by pervasive, but poorly understood, Cenozoic extensional (strike-slip?) faulting of northwest and northeast trend that appears to affect the entire East Siberian-western Chukchi Sea region (for example, Filatova and Khain, 2007;Franke and others, 2004;Kos'ko and others, 1993;Tolson, 1987). Grantz and others (2009).…”
Section: Geologic Setting and Stratigraphymentioning
confidence: 99%
“…Условные обозначения: А -натурная зарисовка рельефа земной поверхности; В -изображение той же земной поверхности геодезистом с помощью горизонталей (1)(2)(3)(4)(5)(6) (на всех топографических картах рельеф земной (почвенной) поверхности представлен такими горизонталями; они образуют физический континуум); С -по выявленным точкам нулевой кривизны проведена морфоизографа (линия нулевой кривизны), закрашено тело положительной литодинамической структуры; D -модель потоковой структуры с особыми точками: R -репеллер, начальная точка движения литовещества; А -аттрактор, точка аккумуляции литовещества; b -точка бифуркации, разветвления потоков…”
Section: материалы и методы исследованияunclassified