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Pyakupur Dome

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Migration of borders of major structures and some subsidiary structures in ...
Published: 01 September 1999
horizon A, 4 – by reflecting horizon B; 5 , 6 – directions of border shifts: 5 – major, 6 – subsidiary. Roman numerals designate major structures : I – Lyamin dome, II – Vyngapur megarampart, III – Yarainer-Etypur megatrough, IV – Yarainer megatrough, V – Nizhnevartovsk dome, VI – South
Journal Article
Published: 01 September 1999
Russ. Geol. Geophys. (1999) 40 (9): 1332–1339.
... horizon A, 4 – by reflecting horizon B; 5 , 6 – directions of border shifts: 5 – major, 6 – subsidiary. Roman numerals designate major structures : I – Lyamin dome, II – Vyngapur megarampart, III – Yarainer-Etypur megatrough, IV – Yarainer megatrough, V – Nizhnevartovsk dome, VI – South...
FIGURES
Journal Article
Published: 01 February 1999
Russ. Geol. Geophys. (1999) 40 (2): 205–215.
..., the South-Muravlenkovo saddle and western Pyakupur trough in the east, and the southwestern flank of the Northern dome in the northeast. Oil and oil-gas-condensate deposits are discovered and explored in the Cretaceous and Upper Jurassic deposits of this area, which lies in the southwestern Nadym-Pur...
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Image
Tectonic map of the northern areas of the Middle Ob’ region by reflecting h...
Published: 01 September 1999
-Yyngayakha Saddle, VI – South-Yyngapur Saddle, VII – Tol’ka megarampart, VIII – Lyamin dome, IX – Nizhnevartovsk dome. Arabic numerals designate subsidiary structures : 1 – Pyakupur domal uplift, 2 – Purpe rampart, 3 – Inguzem rampart, 4 – Etypur rampart, 5 – Vyngayakha rampart, 6 – Vyngapur domal uplift, 7
Image
Tectonic map of the northern areas of the Middle Ob’ region by reflecting h...
Published: 01 September 1999
, III – Nizhnevartovsk dome, IV – South-Muravlenkovo Saddle, V – East-Vyngayakba Saddle, VI – Etypur-Yarainer Saddle, VII – South-Vyngapur Saddle; Arabic numerals, subsidiary structures : 1 – Pyakupur domal uplift, 2 – Purpe rampart, 3 – Inguzem rampart, 4 – Etypur rampart, 5 – Vyngayakba rampart, 6
Journal Article
Published: 01 June 2002
Russ. Geol. Geophys. (2002) 43 (6): 553–566.
... in the Jurassic deposits of West Siberia most promising for oil and gas were under tectonic control [ 24 , 25 ]. These papers state that favorable conditions for the formation of permeable rocks exist on slopes of large positive structures and less favorable conditions, on domes. Since this point of view implies...
FIGURES
Journal Article
Published: 01 December 2002
Russ. Geol. Geophys. (2002) 43 (12): 1107–1123.
.... The slopes of these structures as well as the Khadyr’-Yakha, North Surgut, and Taz monoclines, the within-plate saddles, and the most contrasting bars and domes complicating the large negative structures (megadepressions and megatroughs) promise a moderate potential. The sides of large negative...
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Journal Article
Published: 01 November 2000
Russ. Geol. Geophys. (2000) 41 (11): 1539–1553.
..., Vengapur and Yarainer-Etypur megabars, part of the Nadym depression, and Pyakupur-Amputin megatrough ( Fig. 1 ). The quantitative composition of the studied collection is presented in Table 1 . Fig. 1. Schematic occurrence of sampling localities of oils. 1 – boundaries of major structures; 2...
FIGURES
Journal Article
Published: 01 September 2002
Russ. Geol. Geophys. (2002) 43 (9): 811–825.
... of the Pyakupur dome. The Upper Jurassic section in the core is the most typical of this interval in West Siberia and consists of a sequence of Vasyugan, Georgiev, and Bazhenov Formations. The total thickness of the studied part of the section, combining the Callovian, Upper Jurassic and Lower Cretaceous, is 81.5...
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Journal Article
Published: 01 August 2013
Russ. Geol. Geophys. (2013) 54 (8): 747–779.
... Bol’shaya Kheta megasyneclise. With progressive transgression, the coastal plain gradually migrated southwards along major structures such as the Pyakupur–Amputin and Middle Pur inclined megatroughs and along the northwestern termination of the Yenisei megamonoclise. Oxygen isotope data from belemnite...
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