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Vasyugan Formation

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Journal Article
Published: 01 August 2003
Russ. Geol. Geophys. (2003) 44 (8): 796–808.
... stratigraphy deposition environments facies Jurassic West Siberia Fig. 1. Generalized map of Callovian and Upper Jurassic facies regions in West Siberia and location of SDB-6. 1 — Yamal-Nadym subfacies (Abalak Formation), 2 — Upper Pur subfacies (Vasyugan Formation) of Pur-Irtysh facies; 3...
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Lithology and geophysical characteristics of the <span class="search-highlight">Vasyugan</span> <span class="search-highlight">Formation</span>: A, Ob-...
Published: 01 March 2020
Fig. 3. Lithology and geophysical characteristics of the Vasyugan Formation: A, Ob-Tara sub-region in the Krapivinskaya 201 well, B, Ob-Agan sub-region in the West Sorominskaya 16 well (for well locations see Fig. 2 ). Legend to Figs. 3 , 4 : Gr, Georgievka Formation, TM, Tyumen Formation
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Lithology and geophysical characteristics of the <span class="search-highlight">Vasyugan</span> <span class="search-highlight">Formation</span>, Verkhn...
Published: 01 March 2020
Fig. 4. Lithology and geophysical characteristics of the Vasyugan Formation, Verkhnepur sub-region in the West Novogodnyaya 210 well (for well location see Fig. 2 ).
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Position and stratigraphy of <span class="search-highlight">Vasyugan</span> <span class="search-highlight">Formation</span> in SDB-6 section [ 24 – 26 ...
Published: 01 August 2003
Fig. 3. Position and stratigraphy of Vasyugan Formation in SDB-6 section [ 24 – 26 ]. Q — Quaternary, P — Permian. Rocks: 1 — sandy, 2 — silty, 3 — clayey.
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Time-scale deposition model of <span class="search-highlight">Vasyugan</span> <span class="search-highlight">Formation</span> in SDB-6 section and its ...
Published: 01 August 2003
Fig. 4. Time-scale deposition model of Vasyugan Formation in SDB-6 section and its sequence stratigraphy interpretation. 1 — clay intraclasts; 2 — pyrite nodules; 3 — glauconite; 4 — siderite; 5 — carbonified plant detritus; 6 — flora imprints; 7 — bivalves; 8 — foraminifera; 9
Journal Article
Published: 01 March 2020
Russ. Geol. Geophys. (2020) 61 (3): 330–340.
...Fig. 3. Lithology and geophysical characteristics of the Vasyugan Formation: A, Ob-Tara sub-region in the Krapivinskaya 201 well, B, Ob-Agan sub-region in the West Sorominskaya 16 well (for well locations see Fig. 2 ). Legend to Figs. 3 , 4 : Gr, Georgievka Formation, TM, Tyumen Formation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1993
AAPG Bulletin (1993) 77 (5): 863–887.
... or younger source rocks in the study area. Core samples from the Lower Cretaceous Frolov Formation either are thermally immature (Hauterivian) or show little oil-generative potential (Berriasian-Valanginian). The Upper Jurassic Vasyugan Formation shows lower oil-generative potential than the Bazhenov...
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Journal Article
Published: 01 January 2004
Russ. Geol. Geophys. (2004) 45 (1): 79–90.
...V.A. Kontorovich; S.A. Berdnikova; L.M. Kalinina; A.A. Polyakov A new approach to detection and mapping of oil and gas traps in the Callovian-Tithonian section on the basis of combined seismic, log, and core data has been tested in a field within the Vasyugan Formation. The sand bed U 1 1...
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Cruziana  ichnofacies.   Fig. 1 , Var’eganskaya well, no. 114, depth 2530.7...
Published: 01 October 2011
Plate II. Cruziana ichnofacies. Fig. 1 , Var’eganskaya well, no. 114, depth 2530.7 m, Upper Vasyugan Subformation. Ichnofossils: Pl, Planolites ; Sk, Skolithos ; Pph, Palaeophycus . Fig. 2 , Chernogorskaya well, no. 8, depth 2614.4 m, Vasyugan Formation, Teichichnus ; Fig. 3
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Cruziana–Zoophycos  ichnofacies, escape traces, and deformational bioturbat...
Published: 01 October 2011
Plate III. Cruziana–Zoophycos ichnofacies, escape traces, and deformational bioturbation. Fig. 1 , Var’eganskaya well, no. 114, depth 2521.7 m, Vasyugan Formation, Phycosiphon (Ph); Fig. 2 , Yuzhno-Karasevskaya well, no. 75, depth 2805.5 m, Lower Vasyugan Subformation. Ichnofossils: T
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Skolithos  ichnofacies.   Fig. 1 , Zapadno-Amputinskaya well, no. 33, depth...
Published: 01 October 2011
Plate I. Skolithos ichnofacies. Fig. 1 , Zapadno-Amputinskaya well, no. 33, depth 3196.3 m, Pakhomovskaya Member (bed), Skolithos ; Fig. 2 , Verknechekovskaya well, no. 1, depth 2601.4 m, Vasyugan Formation, intercoal unit, Skolithos ; Fig. 3 , Tyumenskaya SDB-6, depth 3863.3 m, Upper
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Ichnofossil distribution over different types of the Callovian–Oxfordian se...
Published: 01 October 2011
Fig. 5. Ichnofossil distribution over different types of the Callovian–Oxfordian section of the West Siberian basin. A , Vasyugan Formation, Upper Pur facies subregion; B , Vasyugan Formation, Ob’–Tara and Ob’–Agan subregions; C , Abalak Formation; D , Naunak Formation; E , Tochino
Journal Article
Published: 01 December 2001
Russ. Geol. Geophys. (2001) 42 (12): 1806–1816.
.... In the first of them, the Callovian-Oxfordian deposits include the Vasyugan and Abalak Formations; in the second, the Tochino and Sigov Formations; and in the third, the Naunak Formation. Lithological and mineralogo-petrographical studies invoking well logging, geochemistry, and paleontology showed...
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Journal Article
Published: 01 August 2002
Russ. Geol. Geophys. (2002) 43 (8): 762–790.
... grains of terrestrial plants) and bio- and lithostratigraphic features of the uppermost Middle and Upper Jurassic part of the reference section from the Tyumenskaya superdeep borehole. The Vasyugan, Georgiev, and Bazhenov Formations are described in detail, taking into consideration...
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Journal Article
Published: 01 August 2000
Russ. Geol. Geophys. (2000) 41 (8): 1096–1109.
... producing beds, is still much disputed. The article reports correlations between these beds at the level of zonal cyclites. More reliable age analogs of the Bazhenov Formation have been recognized in eastern-type sections. The diachronous nature of the upper boundary of the Vasyugan Formation...
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Pachyteuthis (Pachyteuthis)  cf.  panderiana  (d’Orbigny). Spec. 2017-1, × ...
Published: 01 March 2000
from the top of the range; Oxfordian, Vasyugan Formation. Fig. 2 . Lagonibelus (Holcobeloides) cf. memorabilis (Gustomesov). Spec. 2017-2, × 1: a – ventral outline, b – right profile, c – cross section; Purpe-Vasyugan region, Asomkinskaya BH-1807, depth range 2943–2949, depth 0.8 m from the top
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Fades zoning of the Callovian and Upper Jurasic of the Pur-Irtysb, Taz-Khel...
Published: 01 December 2001
Fig. 2. Fades zoning of the Callovian and Upper Jurasic of the Pur-Irtysb, Taz-Khela, and Sil’ga facies districts of West Siberia. 1 – zone of occurrence of the Abalak Formation (Yamal-Nadym subdistrict of the Pur-Irtysh fades district); 2 – 4 –zone of occurrence of the Vasyugan Formation
Journal Article
Published: 01 March 2001
Russ. Geol. Geophys. (2001) 42 (3): 472–478.
... in the Middle Jurassic deposits suggest that the areas appropriate for hydrocarbon migration from petroleum-generating rocks of the Bazhenov and Togur Formations into Bajocian-Bathonian traps are the most favorable for petroleum deposition. Such are the areas where the marine sediments of the Vasyugan Formation...
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Journal Article
Published: 01 August 1998
Russ. Geol. Geophys. (1998) 39 (8): 1033–1040.
...S. V. Meledina Collections of Middle-Upper Jurassic ammonites found in core samples from West-Siberian boreholes are described. New Upper Callovian species of Longaeviceras and one Lower Oxfordian species of Cardioceras have been discovered in the Abalak and Vasyugan Formations. The small-shell...
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Main types of sections of Upper Jurassic deposits of the Vakh area. A  – Su...
Published: 01 December 2001
Fig. 2. Main types of sections of Upper Jurassic deposits of the Vakh area. A – Survey and exploitation characteristics and B – scheme of relationship between major types of sections of the Vasyugan Formation deposits in the Vakh area. 1 – index of sand strata and coals; 2 – intrareservoir