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Structural map of the Permian surface and tectonic map of the Permian structural tier of the Arctic regions of the Siberian Platform (Khatanga–Lena region). 1 – deep wells, areas; 2 – coastline; 3 – administrative boundary; 4 – zone without Permian deposits, 5 – Verkhoyansk folded region. Tectonic elements: 6–10 – positive structures: 6 – superorder, 7 – I order, 8 – II order, 9 – III order, 10 – IV order; 11–12 – negative structures: 11 – superorder, 12 – I order, 13 – II–III order; 14–16 – intermediate structures: 14 – monoclises, 15 – monolclines, 16 – saddles.

Structural map of the Permian surface and tectonic map of the Permian struc...

Published: 01 June 2024
– monolclines, 16 – saddles. TECTONIC ELEMENTS: Superorder and 0 order: I – East Taimyr monoclise, II – South Laptev syneclise, III – Coastal ridge, IV – Yenisei– Khatanga regional trough, V – Lena–Anabar regional trough, VI – North Anabar megamonoclise; VII – Pre-Verkhoyansk regional trough; Positive
Journal Article

Geology, Oil and Gas Potential, Hydrocarbon Resources and Directions of Geological Exploration in the Northeastern Continental Margin of the Siberian Platform (Anabar–Khatanga and Lena–Anabar OGA)

V.A. Kontorovich, A.E. Kontorovich, L.M. Burshtein, A.Yu. Kalinin, L.M. Kalinina, E.A. Kostyreva, D.S. Melnik, S.A. Moiseev, T.M. Parfenova, P.I. Safronov, M.V. Solovev, A.N. Fomin, E.A. Fursenko
Published: 01 June 2024
Russ. Geol. Geophys. (2024) 65 (6): 714–736.
DOI: https://doi.org/10.2113/RGG20234670
... – monolclines, 16 – saddles. TECTONIC ELEMENTS: Superorder and 0 order: I – East Taimyr monoclise, II – South Laptev syneclise, III – Coastal ridge, IV – Yenisei– Khatanga regional trough, V – Lena–Anabar regional trough, VI – North Anabar megamonoclise; VII – Pre-Verkhoyansk regional trough; Positive...
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View PDF for article title, Geology, Oil and Gas Potential, Hydrocarbon Resources and Directions of Geological Exploration in the Northeastern Continental Margin of the Siberian Platform (<span class="search-highlight">Anabar</span>–Khatanga and <span class="search-highlight">Lena</span>–<span class="search-highlight">Anabar</span> OGA)
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Stratigraphic chart (a) and facies zonation of Jurassic and Cretaceous sediments of the Anabar and adjacent areas (b–e). (a) 1, oil; 2, gas; 3, continental sediments; 4, littoral, lagoonal, and subcontinental sediments; 5, marine sediments; (b) 1, Taimyr–Anabar facies region; 2, Anabar–Olenek facies region; (c), (d) Ob’–Lena facies region: (c) 1, Paksa facies region; 2, Boyarka facies region; 3, Taimyr facies region; 4, Anabar facies region; 5, Anabar–Olenek facies region; (d) 1, Paksa facies region; 2, Taz–Kheta facies region; 3, Taimyr facies region; 4, Lower Lena facies region; (e) Yana–Anabar facies province: 1, Nordvik facies region; 2, East Taimyr facies region; 3, Lena–Anabar facies region.

Stratigraphic chart ( a ) and facies zonation of Jurassic and Cretaceous se...

Published: 01 August 2013
region; 2, Anabar–Olenek facies region; ( c ), ( d ) Ob’–Lena facies region: ( c ) 1, Paksa facies region; 2, Boyarka facies region; 3, Taimyr facies region; 4, Anabar facies region; 5, Anabar–Olenek facies region; ( d ) 1, Paksa facies region; 2, Taz–Kheta facies region; 3, Taimyr facies region; 4
Journal Article

Seismogeologic, Structural, and Tectonic Characteristics of the Continental Margin of the Siberian Platform (Khatanga–Lena Interfluve)

V.A. Kontorovich, A.E. Kontorovich, A.Yu. Kalinin, L.M. Kalinina, V.V. Lapkovskii, B.L. Lunev, S.A. Moiseev, M.V. Solovev
Published: 01 August 2021
Russ. Geol. Geophys. (2021) 62 (08): 947–963.
DOI: https://doi.org/10.2113/RGG20214352
..., are considered. Vendian. In the Anabar–Khatanga and Lena–Anabar OGAs, Vendian deposits are unconformably overlain on the Riphean and are composed of carbonates. In the east of the Khatanga–Lena region, in the upper part of the Vendian–lower Cambrian, there is a stratum of terrigenous rocks...
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View PDF for article title, Seismogeologic, Structural, and Tectonic Characteristics of the Continental Margin of the Siberian Platform (Khatanga–<span class="search-highlight">Lena</span> Interfluve)
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A schematic map of the Yakutian diamondiferous province with elements of oil-geological zoning. Boundary of: 1 — petroliferous provinces, 2 — petroliferous regions, 3 — Yakutian diamondiferous province. Petroliferous regions: Lena-Vilyui PP: LA — Lena-Anabar, CV — Cis-Verkhoyansk, V — Vilyui; Lena-Yenisei PP: NB — Nepa-Botuobiyan, CP — Cis-Patom, WV — West Vilyui, NA — North Aldan, S — Syugdzher, K — Kureika, A — Anabar.

A schematic map of the Yakutian diamondiferous province with elements of oi...

Published: 01 February 2005
Fig. 1. A schematic map of the Yakutian diamondiferous province with elements of oil-geological zoning. Boundary of: 1 — petroliferous provinces, 2 — petroliferous regions, 3 — Yakutian diamondiferous province. Petroliferous regions: Lena-Vilyui PP: LA — Lena-Anabar, CV — Cis-Verkhoyansk, V
Image
Correlation of sections (А), facies zoning (B), comparison of formations in different facies zones (C), thickness changes (D) Bathonian– Neocomian sections of the Anabar–Lena sedimentary basin and paleogeography of the Anabar–Lena region at the end of the Late Jurassic and beginning of the Cretaceous (E). 1–2 – boundaries: 1 – formations; 2 – stages; 3 – boundaries of facies areas; 4 – section correlation line (а), studied sections (b) (B, E). For the rest of the information, see Fig. 2.

Correlation of sections ( А ), facies zoning ( B ), comparison of formation...

Published: 01 November 2023
Fig. 4. Correlation of sections ( А ), facies zoning ( B ), comparison of formations in different facies zones ( C ), thickness changes ( D ) Bathonian– Neocomian sections of the Anabar–Lena sedimentary basin and paleogeography of the Anabar–Lena region at the end of the Late Jurassic
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Facies zonation of Triassic deposits in the northern Central Siberia (modified after Kazakov et al., 2002). Boundaries of: 1, facies areas; 2, facies regions. Facies areas: I, Taimyr; II, Khatanga–Lower Lena; III, Kotuy–May-mecha; IV, Lena–Lower Vilyuy; V, Kotelny–Bennet. Facies regions: 1, Tulay-Kiryak; 2, East Taimyr; 3, Ust’-Anabar; 4, Lena–Olenek; 5, Buur–Olenek; 6, Lower Lena; 7, Kharaulakh; 8, Orulgan.

Facies zonation of Triassic deposits in the northern Central Siberia (modif...

Published: 01 August 2013
regions: 1, Tulay-Kiryak; 2, East Taimyr; 3, Ust’-Anabar; 4, Lena–Olenek; 5, Buur–Olenek; 6, Lower Lena; 7, Kharaulakh; 8, Orulgan.
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Tectonic scheme of the Siberian Platform cover (according to [2].with author’s additions). 1 – modern boundaries of the Siberian Platform (a – reliable, b – supposed), confined chiefly to zones of deep faults; 2 – major frontal overthrusts of the marginal zones of the platform; 3 – main zones of intracratonic faults; boundaries: 4 – largest (superrank) and 5 – separate large (first rank) plicative structures of various signs. The largest structures are: I – Yenisei-Khatanga regional trough, II – pre-Verkhoyansk marginal trough; III – Vlyui hemisyneclise; IV – Anabar, V – Aldan, VI – Nepa-Botuoba, and VII – Baikit anteclises; VIII – Kureika syneclise; IX – Sayan-Yenisei Syneclise; X – pre-Patom regional trough; XI – Angara-Lena step. Major features: 1 – Khantaika-Rybninsk megarampart, 2 – Kureika-Baklanikha megarampart, 3 – Anabar-Khatanga saddle, 4 – Lena-Anabar megatrough, 5 – Ygyatta depression, 6 – Kempendyai depression, 7 – Suntara arch, 8 – Syugdzher saddle, 9 – Katanga saddle.

Tectonic scheme of the Siberian Platform cover (according to [ 2 ].with aut...

Published: 01 August 1996
– Aldan, VI – Nepa-Botuoba, and VII – Baikit anteclises; VIII – Kureika syneclise; IX – Sayan-Yenisei Syneclise; X – pre-Patom regional trough; XI – Angara-Lena step. Major features: 1 – Khantaika-Rybninsk megarampart, 2 – Kureika-Baklanikha megarampart, 3 – Anabar-Khatanga saddle, 4 – Lena-Anabar
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Map of Vendian-Lower Cambrian petroleum-promising subsalt fields and petroleum-geological regionalization of the Siberian Platform, after [7]. Fields: 1 – oil, 2 – oil-gas and gas-oil, 3 – gas and gas-condensate; 4 – bitumen fields. Petroleum-promising deposits: 5 – of rank I, 6 – of rank II, 7 – of rank III, 8 – low-grade, 9 – presumably high-grade, 10 – unpromising. Boundaries of: 11 – petroliferous provinces (A – Lena-Tunguska, B – Khatanga-Vilyui), 12 – areas of differently promising deposits, 13 – high-rank structures; 14 – overthrust zones with contours of allochthon structures; 15 – marginal sutures of the platform. Fields: 1 – Deryabinskoe, 2 – Soleninskoe, 3 – Srednetyungskoe, 4 – Sredne-vilyuiskoe, 5 – Tolon-Mastakhskoe, 6 – Solobokh-Nedzhelinskoe, 7 – Sobinskoe, 8 – Irelyakhskoe, 9 – Srednebotuobinskoe, 10 – Verkhnevilyuchanskoe, 11 – Verkhnechon- skoe, 12 – Danilovskoe, 13 – Dulisminskoe, 14 – Yaraktinskoe, 15 – Markovskoe, 16 – Yurubchenskoe. Tectonic elements: I – Yenisei-Khatanga regional trough, II – Anabar-Khatanga saddle, III – Lena-Anabar megatrough, IV – cis-Verkhoyansk marginal trough, V – Vilyui hemisyneclise, VI – Aldan anteclise, VII – cis-Patom regional trough, VIII – Nepa-Botuobiyan anteclise, IX – Angara-Lena structural stage, X – Katanga saddle, XI – Sayan-Yenisei syneclise, XII – Baikit anteclise, XIII – Kureika syneclise, XIV – Anabar anteclise, XV – Syugdzher saddle.

Map of Vendian-Lower Cambrian petroleum-promising subsalt fields and petrol...

Published: 01 April 2001
– Verkhnechon- skoe, 12 – Danilovskoe, 13 – Dulisminskoe, 14 – Yaraktinskoe, 15 – Markovskoe, 16 – Yurubchenskoe. Tectonic elements : I – Yenisei-Khatanga regional trough, II – Anabar-Khatanga saddle, III – Lena-Anabar megatrough, IV – cis-Verkhoyansk marginal trough, V – Vilyui hemisyneclise, VI – Aldan
Journal Article

Lower Cretaceous biostratigraphy of Northern Siberia: palynological units and their correlation significance

E.B. Pestchevitskaya
Published: 01 November 2007
Russ. Geol. Geophys. (2007) 48 (11): 941–959.
DOI: https://doi.org/10.1016/j.rgg.2007.10.004
... assemblages with similar systematic compositions were reported from Berriasian sections of the Subarctic Urals, the Khatanga basin, and the Lena-Anabar region: the spore-pollen compositions change above the base of the Hectoroceras kochi Zone to include many Upper Berriasian and Lower Valanginian taxa...
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Journal Article

Detailed Geoseismic Structure of the Riphean Deposits in Buolkalakh–Lena Area Based on Deep Drilling and Seismic Exploration Data

D.S. Lezhnin, M.A. Maslennikov
Published: 01 June 2023
Russ. Geol. Geophys. (2023) 64 (6): 724–734.
DOI: https://doi.org/10.2113/RGG20234552
... of the Lena–Anabar trough. The region also developed older Riphean deposits that are not exposed on the Olenek uplift and are not studied by deep drilling. The prospects for the oil and gas content of Riphean strata in the region are mainly associated with carbonate reservoirs formed in the top of the Riphean...
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View PDF for article title, Detailed Geoseismic Structure of the Riphean Deposits in Buolkalakh–<span class="search-highlight">Lena</span> Area Based on Deep Drilling and Seismic Exploration Data
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Journal Article

Thermal Conductivity of Rocks and Estimates of Heat Flow in the Lena–Anabar Interfluve (Siberian Platform)

A.D. Duchkov, D.E. Ayunov, P.A. Yan, A.I. Sivtsev, L.S. Sokolova
Published: 01 June 2023
Russ. Geol. Geophys. (2023) 64 (6): 713–723.
DOI: https://doi.org/10.2113/RGG20224518
... in other northern regions of Siberia for obtaining more geothermal data. wells physical properties of rocks thermograms of wells heat flow Siberian Platform Lena–Anabar interfluve Juxtaposition of all λ d and φ values of the samples showed a linear correlation between these parameters...
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View PDF for article title, Thermal Conductivity of Rocks and Estimates of Heat Flow in the <span class="search-highlight">Lena</span>–<span class="search-highlight">Anabar</span> Interfluve (Siberian Platform)
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Oil- and gas-bearing regions of the Siberian Platform. Oi1- and gas-bearing regions (encircled). A – Lena-Tunguska OGP: 1 – Turukhan-Norilsk, 2 – North-Tunguska, 3 – Anabar, 4 – South-Tunguska, 5 – Syugdzber, 6 – West-Vilyui, 7 – North-Aldan, 8 – Baikit, 9 – Katanga, 10 – Nepa-Botuoba, 11 – pre-Patom, 12 – Sayan-Yenisei, 13 – Angara-Lena; B – Khatanga-Vilyui OGP: 14 – Yenisei-Khatanga, 15 – Anabar-Khatanga, 16 – Lena-Anabar, 17 – pre-Verkhoyansk, 18 – Vilyui. Oil and gas deposits. The Lena-Tunguska OGP: 1 – Moktakonskoe, 2 – Yurubchenskoe, 3 – Terskoe, 4 – Ust’-Kuyumbinskoe, 5 – Sredne-Kuyumbinskoe, 6 – Sobinskoe, 7 – Paiginskoe, 8 – Bratskoe, 9 – Atovskoe, 10 – Kovyktinskoe, 11 – Markovskoe, 12 – Yaraktinskoe, 13 – Ayanskoe, 14 – Dulisminskoe, 15 – Danilovskoe, 16 – Preobrazhenskoe, 17 – Verkhne - Chonskoe, 18 – Vakunaiskoe, 19 – Talakonskoe, 20 – Nizhne-Khamakinskoe, 21 – Chayandinskoe, 22 – Sredne-Botuobinskoe, 23 – Tas-Yuryakhskoe, 24 – Iktekhskoe, 25 – Verkhne-Vilyuchanskoe, 26 – Vilyuisko-Dzherbinskoe, 27 – Machchobinskoe, 28 – Ir-elyakhskoe, 29 – Mirninskoe, 30 – Nelbinskoe, 31 – Bysakhtakhskoe, 32 – Omorinskoe; the Khatanga-Vilyui OGP: 33 – Zimnee, 34 – Messoyakhskoe, 35 – Yuzhno-Soleninskoe, 36 – Severo-Soleninskoe, 37 – Ushakovskoe, 38 – Nandyanskoe, 39 – Pelyatkinskoe, 40 – Kazantsevskoe, 41 – Ozernoe, 42 – Payakhskoe, 43 – Deryabinskoe, 44 – Khabeiskoe, 45 – Balakhninskoe, 46 – Andylakhskoe, 47 – Sredne-Tyungskoe, 48 – Nizhne-Tyukyanskoe, 49 – Sredne-Vilyuiskoe, 50 – Tolon-Mastakhskoe, 51 – Sobolokh-Nedzhelinskoe, 52 – Badarnskoe, 53 – Nizhne-Vilyuiskoe, 54 – Ust’-VUyuiskoe, 55 – Sobo-Khainskoe.

Oil- and gas-bearing regions of the Siberian Platform. Oi1- and gas-bearing...

Published: 01 August 1996
Fig. 1. Oil- and gas-bearing regions of the Siberian Platform. Oi1- and gas-bearing regions (encircled). A – Lena-Tunguska OGP : 1 – Turukhan-Norilsk, 2 – North-Tunguska, 3 – Anabar, 4 – South-Tunguska, 5 – Syugdzber, 6 – West-Vilyui, 7 – North-Aldan, 8 – Baikit, 9 – Katanga, 10 – Nepa-Botuoba
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Location of the Lower Cambrian key sections of the Siberian Platform. 1, location of the Lower Cambrian key sections: I, Lena River (middle reaches); II, Lena River (lower reaches, Kharaulakh Mts.); III, Olenek uplift (Khorbosuonka River); IV, Nekekit River (northeastern Siberian Platform); V, western Anabar region (Medvezh’ya and Eriechka River basins); VI, Sukharikha River (northwestern Siberian Platform); 2, Siberian Platform boundary.

Location of the Lower Cambrian key sections of the Siberian Platform. 1 , ...

Published: 01 July 2011
Platform); V, western Anabar region (Medvezh’ya and Eriechka River basins); VI, Sukharikha River (northwestern Siberian Platform); 2 , Siberian Platform boundary.
Journal Article

The lower boundary of the Toyonian stage (Cambrian) of the Siberian Platform

I.V. Korovnikov
Published: 01 July 2011
Russ. Geol. Geophys. (2011) 52 (7): 717–724.
DOI: https://doi.org/10.1016/j.rgg.2011.06.004
... Platform); V, western Anabar region (Medvezh’ya and Eriechka River basins); VI, Sukharikha River (northwestern Siberian Platform); 2 , Siberian Platform boundary. ...
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Map of the Siberian platform with location of sections referred to in the text. Sections: Al, Aldan; Ko, western Anabar region (Kotuj and Kotujkan rivers); Ku, Bol’shaya Kuonamka; Le, Lena (middle reaches); Se, Selinde. Facies belts: 1, lagoonal; 2, transitional; 3, normal-marine.

Map of the Siberian platform with location of sections referred to in the t...

Published: 01 July 2005
Figure 1. Map of the Siberian platform with location of sections referred to in the text. Sections: Al, Aldan; Ko, western Anabar region (Kotuj and Kotujkan rivers); Ku, Bol’shaya Kuonamka; Le, Lena (middle reaches); Se, Selinde. Facies belts: 1, lagoonal; 2, transitional; 3, normal-marine.
Journal Article

Stratigraphy and Sedimentogenesis of the Clinoform Upper Jurassic of the Anabar–Lena Sedimentary Basin (Arctic Siberia, Laptev Sea Coast)

V.P. Devyatov, B.L. Nikitenko
Published: 01 November 2023
Russ. Geol. Geophys. (2023) 64 (11): 1347–1357.
DOI: https://doi.org/10.2113/RGG20234620
...Fig. 4. Correlation of sections ( А ), facies zoning ( B ), comparison of formations in different facies zones ( C ), thickness changes ( D ) Bathonian– Neocomian sections of the Anabar–Lena sedimentary basin and paleogeography of the Anabar–Lena region at the end of the Late Jurassic...
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View PDF for article title, Stratigraphy and Sedimentogenesis of the Clinoform Upper Jurassic of the <span class="search-highlight">Anabar</span>–<span class="search-highlight">Lena</span> Sedimentary Basin (Arctic Siberia, Laptev Sea Coast)
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Tectonic map of the Siberian platform Arctic regions (Khatanga–Lena interfluve). 1, deep wells, areas, 2, coastline, 3, rivers, 4, Khatanga–Lena (Ust’-Olenek) zone, 5, settlements, 6, administrative border, 7, zone of no Permian deposits, 8, Verkhoyansk folded region; tectonic elements: positive structures: 9, superorder, 10, order I, 11, order II, 12, order III, 13, order IV; negative: 14, superorder, 15, order I, 16, order II—III; intermediate structures: 17, monoclises, 18, monoclines, 19, mesosaddles.

Tectonic map of the Siberian platform Arctic regions (Khatanga–Lena interfl...

Published: 01 August 2021
monoclise, II, South Laptev syneclise, III, Coastal Ridge, IV, Yenisei–Khatanga regional trough, V, Lena–Anabar syneclise, VI, North Anabar megamonoclise; VII, Predverkhoyansk regional trough; Positive structures: order I (megaswell, megawedge, arch): I, Pritaimyr megawedge, II, Yuryang megaswell, III
Journal Article

Organic Geochemistry of Carbonate Rocks, Silicites and Black Shales of the Vendian (Ediacaran) Khatyspyt Formation, Northeastern Siberia

D.S. Melnik, T.M. Parfenova, D.V. Grazhdankin, V.I. Rogov
Published: 01 June 2023
Russ. Geol. Geophys. (2023) 64 (6): 698–712.
DOI: https://doi.org/10.2113/RGG20224527
... ; Kontorovich et al., 1995 ; Kashirtsev, 2003 ; Peters et al., 2005 ; Parfenova et al., 2010 ; Duda et al., 2020 ). According to the modern notion based on regional geological survey and seismic data the Neoproterozoic deposits dip to the west (Sukhana Depression), the north and the east (Lena–Anabar...
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View PDF for article title, Organic Geochemistry of Carbonate Rocks, Silicites and Black Shales of the Vendian (Ediacaran) Khatyspyt Formation, Northeastern Siberia
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Journal Article

The Neoproterozoic–Phanerozoic section of the Anabar–Lena province: structural framework, geological model, and petroleum potential

V.A. Kontorovich, A.E. Kontorovich, I.A. Gubin, A.M. Zoteev, V.V. Lapkovsky, N.A. Malyshev, M.V. Soloviev, G.S. Fradkin
Published: 01 August 2013
Russ. Geol. Geophys. (2013) 54 (8): 980–996.
DOI: https://doi.org/10.1016/j.rgg.2013.07.014
... , regional composite CMP profiles; 3 , deep wells. However, synthesis and comprehensive interpretation of the data collected in the 1980s was impossible because of the political and economic crisis of the 1990s. The data from the wells in the Anabar–Lena province ( Fig. 2 ) can be summarized...
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View PDF for article title, The Neoproterozoic–Phanerozoic section of the <span class="search-highlight">Anabar</span>–<span class="search-highlight">Lena</span> province: structural framework, geological model, and petroleum potential
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