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Churbiga Formation

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Group composition of the autochthonous Vendian–Cambrian chloroform extracts...
Published: 01 June 2011
; 6 , Churbiga Formation; 7 – 11 , chloroform extracts from the well Vostok-3: 7 , Paidugina Formation; 8 , Churbiga Formation; 9 , Raiga Formation; 10 , Kotodzha Formation; 11 , Poiga Formation; 12 , 13 , areas of the group composition of the allochthonous chloroform extracts from the wells
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Chromatograms of the  n -alkanes and mass chromatograms of the  n -alkanes ...
Published: 01 June 2011
Fig. 3. Chromatograms of the n -alkanes and mass chromatograms of the n -alkanes ( m / z = 71), monomethylalkanes ( m / z = 182), and cyclohexanes ( m / z = 83) from the Cambrian autochthonous chloroform extracts of the Cis-Yenisei subprovince. a , Churbiga Formation, Vostok-3, 3808.56 m
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Geological and geophysical cross section of Cambrian deposits in Vostok-1 w...
Published: 01 November 2008
. Pd — Paidugina Formation, Chr — Churbiga Formation.
Journal Article
Published: 01 June 2011
Russ. Geol. Geophys. (2011) 52 (6): 571–582.
...; 6 , Churbiga Formation; 7 – 11 , chloroform extracts from the well Vostok-3: 7 , Paidugina Formation; 8 , Churbiga Formation; 9 , Raiga Formation; 10 , Kotodzha Formation; 11 , Poiga Formation; 12 , 13 , areas of the group composition of the allochthonous chloroform extracts from the wells...
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Journal Article
Published: 01 November 2008
Russ. Geol. Geophys. (2008) 49 (11): 843–850.
.... Pd — Paidugina Formation, Chr — Churbiga Formation. ...
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Journal Article
Published: 01 May 2014
Russ. Geol. Geophys. (2014) 55 (5-6): 704–715.
... ; Kontorovich and Savitskii, 1970 ; Mel’nikov et al., 1989 ; Pisarchik et al., 1975 ; and others). Fig. 2. Seismic section along the Vostok-10 regional profile. Formations and series: us, Usolka; oks, Oksym; t, Tyya; av, Averin; kl, Kol’chum; el, Elogui; ch, Churbiga; pd, Paidugina; pud, Pudzhelga; pod...
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Journal Article
Published: 01 December 2008
Russ. Geol. Geophys. (2008) 49 (12): 932–939.
.... Overlying carbonate deposits of the Kotodzha Formation containing alumino-siliciclastics and chert interlayers are interpreted as the fore-reef slope and reef-foot facies. Deposition by turbidity currents is further observed upsection (Raiga Formation). A fine-grained texture of the Churbiga and Paidugina...
FIGURES
Journal Article
Published: 01 July 2023
Russ. Geol. Geophys. (2023) 64 (7): 839–846.
... of insoluble organic matter (kerogen) from Cambrian deposits of the southern cis-Yenisei subbasin Well Sampling depth, m Age Formation Rock δ 13 C, ‰ Vostok-3 3808.6 Є 1 Nizhnyaya Churbiga calcareous mudstone –33.0 Vostok-3 3807.4 Є 1 Nizhnyaya Churbiga calcareous mudstone –34.4...
FIGURES
Journal Article
Published: 01 June 2015
Russ. Geol. Geophys. (2015) 56 (6): 919–931.
... of the Averinskaya-150 and Lemok-1 wells ( Fig. 1 ). Coeval formations were distinguished: the Oksym Formation, in the Vostok-4 well; the Churbiga Formation (lower part), in the Vostok-3 well; the Lisitsa Series (volcanosedimentary part of the Lower Cambrian section in the Vezdekhodnaya area), in the Vezdekhodnaya-4...
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Journal Article
Published: 01 March 2021
Russ. Geol. Geophys. (2021) 62 (03): 357–376.
... decreases considerably. The coeval sediments of the Usolka and Oksym Formations are here correlated with the lower unit of the Churbiga Formation (Vostok-1 and Vostok-3). The age correlation with the western parts of the Siberian Platform and western part of the Yenisei Ridge is similar to that of the above...
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Seismic section along the Vostok-10 regional profile. <span class="search-highlight">Formations</span> and series...
Published: 01 May 2014
Fig. 2. Seismic section along the Vostok-10 regional profile. Formations and series: us, Usolka; oks, Oksym; t, Tyya; av, Averin; kl, Kol’chum; el, Elogui; ch, Churbiga; pd, Paidugina; pud, Pudzhelga; pod, Podelga; kn, Kondes; sh, Shedelga; pn, Pyzhina; ev, Evenki; bl, Belaya.
Journal Article
Published: 24 December 2024
Russ. Geol. Geophys. (2024)
... specific features of TOC distribution, isotopic and elemental compositions of kerogen from the Cambrian formations, several stratigraphic levels enriched in organic matter that has undergone substantial transformation (suggesting a high level of its maturity) were recognized as a bed in the Churbiga Fm (Є...
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Relationship between the bitumoid coefficient (β) and content of organic ca...
Published: 24 December 2024
water salinity, Formations: 7 – Elogui; 8 – Maloe Omutli, 9 – Evenki; Open sea shelf and continental slope with primary productivity ranking as: “Normal”, Facies type 4, Formations: 10 – Churbiga; 11 – Pudzhelga, 12 – Podelga, 13 – Kondes, 14 –Shedelga; high, Facies type 5: 15
Journal Article
Published: 01 April 2015
Russ. Geol. Geophys. (2015) 56 (4): 560–572.
... shale of the Churbiga Formation containing fragmented skeletal fossils of Cambrian age. The total intersected thickness of the Vendian comprises 1132 m. In the east of the Fore-Yenisei Basin , the Vendian is thought to be reached by the Averinskaya-150 Borehole. Lithological similarity...
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Regional seismic profile Vostok-10 of the Fore-Yenisei sedimentary basin. L...
Published: 01 April 2015
siliciclastic–sulphate–dolostone evaporitic complex; 4 , Lower Cambrian chert–mudstone–carbonate carbonaceous stagnant complex (Churbiga and Paidugina Formations); 5 , Lower Cambrian sulphate–carbonate and sulphate–carbonate–saliferous evaporitic complex (Usolye Formation); 6, bioherm complex ( a , Poiga
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Index fossils of Vendian and Cambrian age from the Borehole Vostok 3.  a–e ...
Published: 01 December 2008
Fig. 3. Index fossils of Vendian and Cambrian age from the Borehole Vostok 3. a–e — Namacalathus sp.: a , b — Kotodzha Formation (depth 4412–4405 m), c , d — Lower Raiga Member (depth 4161–4149 m), e — Middle Raiga Member (depth 4061–4054 m); f , g — calcareous sponge spicules
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Correlation of sections of the Usolka, Oksym, <span class="search-highlight">Churbiga</span>, and Lebyazh’e Forma...
Published: 01 June 2015
Fig. 1. Correlation of sections of the Usolka, Oksym, Churbiga, and Lebyazh’e Formations within the Cis-Yenisei sedimentary basin, supplemented and modified after ( Filippov et al., 2014 ). 1–5, limestones: 1, with no admixtures, massive; 2, lumpy; 3, stromatolite (a, Sheet; b, columnar); 4
Journal Article
Published: 01 April 2017
Russ. Geol. Geophys. (2017) 58 (3-4): 371–383.
... Early Cambrian sequence reduces in the same direction (it was stripped by wells Vostok-3 and Vostok-1 in the west where it consists of the ~200 m thick Churbiga Formation). Fig. 5. Seismic-geological cross section along composite profile Vostok-16a and Batolit transect. Legend same as in Fig...
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