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Inikan Formation

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Journal Article
Published: 01 February 2024
Russ. Geol. Geophys. (2024) 65 (2): 251–271.
...S.I. Merenkova; G.A. Kalmykov; A.Yu. Puzik; R.R. Gabdullin; I.V. Bad’yanova; M.A. Volkova; K.P. Kazymov; M.M. Shiroyan Abstract —Geochemical studies of Inikan Formation rocks from the coastal outcrops of the Yudoma River were carried out. All analyzed lithological varieties are characterized...
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Barite and apatite in rocks of the Inikan Formation. а – barite surrounded by OM, b – organic remains replaced by phosphate, surrounded by OM, and barite; c, d – algae (?) replaced by apatite.
Published: 01 February 2024
Fig. 4. Barite and apatite in rocks of the Inikan Formation. а – barite surrounded by OM, b – organic remains replaced by phosphate, surrounded by OM, and barite; c , d – algae (?) replaced by apatite.
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Trace elements contents in the Inikan Formation rocks for: 1 – lydite (smp. G03-001), 2 – mudstone (smp. G05-035), 3 – limestone (smp. G06-40), in comparison with trace elements contents in seawater, with the plot built after (Holland, 1979).
Published: 01 February 2024
Fig. 9. Trace elements contents in the Inikan Formation rocks for: 1 – lydite (smp. G03-001), 2 – mudstone (smp. G05-035), 3 – limestone (smp. G06-40), in comparison with trace elements contents in seawater, with the plot built after ( Holland, 1979 ).
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Paleosection along profile 080321a for the origin of the Inikan Formation.
Published: 01 May 2014
Fig. 7. Paleosection along profile 080321a for the origin of the Inikan Formation.
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Time CDP section along profiles 080321 and 080321a. 1, boundaries of the Inikan Formation and Khochom rock unit; 2, boundaries of formations: tt, Totta; sw, Svetlaya; tl, Talyn; chs, Chaya; in, Inikan; ps, Pestrotsvetnaya; ujg, Ust’-Yudoma; om-gn, Omakhta-Gonam (undivided); us-ms, Ust’-Maya; in, Inikan Formation; ps, Pestrotsvetnaya; hch, Khochom rock unit; F, basement.
Published: 01 May 2014
Fig. 6. Time CDP section along profiles 080321 and 080321a. 1 , boundaries of the Inikan Formation and Khochom rock unit; 2 , boundaries of formations: tt, Totta; sw, Svetlaya; tl, Talyn; chs, Chaya; in, Inikan; ps, Pestrotsvetnaya; ujg, Ust’-Yudoma; om-gn, Omakhta-Gonam (undivided); us-ms, Ust
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Location of the points for the compositions of terrigenous rocks of the Inikan Formation in the (A–CN–K) and CIA-Kcorr diagrams, after (Fedo et al., 1995).
Published: 01 February 2024
Fig. 10. Location of the points for the compositions of terrigenous rocks of the Inikan Formation in the (A–CN–K) and CIA-K corr diagrams, after ( Fedo et al., 1995 ).
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Seismic time section along the composite profile 080314+080316 (Khandygskaya prospect). Indices of seismic reflectors: Rlh – base of the Lakhanda Group, Rnr – top of the Neryuen Formation, Rig – top of the Ignikan Formation, VR –base of the Vendian, K2 – base of the Inikan Formation. Indices of other reflectors are shown in Fig. 2. Indices of seismic sequences corresponding to the Riphean groups and formations are shown in Fig. 5.
Published: 01 January 2024
Fig. 9. Seismic time section along the composite profile 080314+080316 (Khandygskaya prospect). Indices of seismic reflectors: Rlh – base of the Lakhanda Group, Rnr – top of the Neryuen Formation, Rig – top of the Ignikan Formation, VR –base of the Vendian, K 2 – base of the Inikan Formation
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Geologic section of the Khochomskaya well 1. 1, limestones; 2, dolomites; 3, clayey limestones; 4, organogenic limestones; dolomites; 5, marls; 6, mudstones; 7, siltstones; 8, sandstones; 9, basement rocks; 10, cavernosity; 11, bituminosity; 12, Pestrotsvetnaya Formation; 13, Inikan Formation; 14, Aldan Superstage; 15, Lena Superstage.
Published: 01 May 2014
Formation; 13 , Inikan Formation; 14 , Aldan Superstage; 15 , Lena Superstage.
Journal Article
Published: 01 May 2014
Russ. Geol. Geophys. (2014) 55 (5-6): 619–628.
...Fig. 7. Paleosection along profile 080321a for the origin of the Inikan Formation. ...
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Schematic occurrence of stylolites in carbonate rocks of the productive member of the Sardana Formation at the Sardana deposit. 1 – observation point (borehole) and number of stylolites per meter of the productive-member thickness; 2 – isolines of equal contents of stylolites; 3 – geologic boundaries; 4 – dips and strikes; 5 – orebodies; encircled “S” – Sardana syncline; encircled “K” – Kurung anticline; R3uk – Upper Riphean, Ust’-Kirba Formation; Vjd – Vendian, Yudoma series; ϵ1 – Lower Cambrian, Pestrotsvetnaya and Inikan Formations; ϵ2 – Middle Cambrian, Chaya and Ust’-Maya Formations.
Published: 01 March 2001
– geologic boundaries; 4 – dips and strikes; 5 – orebodies; encircled “S” – Sardana syncline; encircled “K” – Kurung anticline; R 3 uk – Upper Riphean, Ust’-Kirba Formation; Vjd – Vendian, Yudoma series; ϵ 1 – Lower Cambrian, Pestrotsvetnaya and Inikan Formations; ϵ 2 – Middle Cambrian, Chaya and Ust
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Schematic occurrence of oil source horizons and reservoirs in the sedimentary cover of the Aldan–Maya depression. 1, oil source horizons; 2, reservoirs: a, granular, b, fracture-cavernous. Stratigraphic units: R1–2, Lower–Middle Riphean deposits of the Aimchan and Uchur Groups and their age analogs; R2tt, Middle Riphean Totta Formation; R2ms, Middle Riphean Muskel’ Formation; R2ml, Middle Riphean Malgin Formation; R2zp, Middle Riphean Tsipanda Formation; R3nr, Upper Riphean Neryuen Formation; R3ig, Upper Riphean Ignikan Formation; R3us, Upper Riphean Ust’-Kirba Group; Vsr, Vendian Sardana Formation; Vjuk, Vendian Yukanda Formation; Є1ps, Lower Cambrian Pestrotsvetnaya Formation; Є1–2in, Lower–Middle Cambrian Inikan Formation; Є2m, Middle Cambrian Mayan deposits.
Published: 01 April 2017
, Vendian Sardana Formation; Vjuk, Vendian Yukanda Formation; Є 1 ps, Lower Cambrian Pestrotsvetnaya Formation; Є 1–2in , Lower–Middle Cambrian Inikan Formation; Є 2 m, Middle Cambrian Mayan deposits.
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Scheme of facies zonation of Cambrian deposits (Botomian Stage) based on the results of deep drilling and interpretation of seismic data. 1, major basement highs (zones where the Cambrian is absent); 2, zone of absence of the Inikan Formation, as indicated by seismic data; 3–6, salt basin facies: 3, penetrated by wells, 4, predicted from seismic data, 5, mapped based on drilling and seismic data, 6, inferred; 7–10, barrier-reef facies: 7, penetrated by wells, 8, mapped from seismic data, 9, mapped from drilling and seismic data, 10, inferred; 11–15, open basin facies: 11, penetrated by wells, 12, mapped from seismic data, 13, predicted from seismic data, 14, mapped from drilling and seismic data, 15, inferred; 16, massive body-type anomalies of the wave field. Abbreviated names of formations and strata: SK, Sinyaya-Kutorgina, Ud, Udachnaya, Ol, Olekma, Km, Kumakh. For wells abbreviations see Fig. 1.
Published: 01 August 2021
Fig. 9. Scheme of facies zonation of Cambrian deposits (Botomian Stage) based on the results of deep drilling and interpretation of seismic data. 1 , major basement highs (zones where the Cambrian is absent); 2 , zone of absence of the Inikan Formation, as indicated by seismic data; 3–6 , salt
Journal Article
Published: 01 August 2021
Russ. Geol. Geophys. (2021) 62 (08): 914–928.
...Fig. 9. Scheme of facies zonation of Cambrian deposits (Botomian Stage) based on the results of deep drilling and interpretation of seismic data. 1 , major basement highs (zones where the Cambrian is absent); 2 , zone of absence of the Inikan Formation, as indicated by seismic data; 3–6 , salt...
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Journal Article
Published: 01 January 2024
Russ. Geol. Geophys. (2024) 65 (1): 5–19.
..., the industrial oil content of the Kuonam and Inikan formations deposits has not been established to date due to the extremely low degree of study and lack of testing. Domanik pay deposits are part of the same age carbonate formations and are relatively deep-water analogues of shallow shelf carbonates...
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Journal Article
Published: 01 January 2024
Russ. Geol. Geophys. (2024) 65 (1): 111–125.
... often not reported. kerogen kinetic characteristics of kerogen Kuonamka Formation Inikan Formation Cambrian In the context of a paradigm shift in the development of the Russia’s oil and gas industry, the focus of regional and exploration activities moves toward the eastern and northern...
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Journal Article
Published: 01 May 2014
Russ. Geol. Geophys. (2014) 55 (5-6): 755–762.
...–400 mg HC/g TOC, measured on early mature source rocks ( T max ≤ 435 °C). The deposits of the Lower–Middle Cambrian Kuonamka and Inikan Formations , studied in the exposures of the Molodo, Yudoma, and Maya Rivers, are composed of alternating dark-colored limestones, marls, mudstones, and clay...
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Journal Article
Published: 01 April 2017
Russ. Geol. Geophys. (2017) 58 (3-4): 529–540.
..., Vendian Sardana Formation; Vjuk, Vendian Yukanda Formation; Є 1 ps, Lower Cambrian Pestrotsvetnaya Formation; Є 1–2in , Lower–Middle Cambrian Inikan Formation; Є 2 m, Middle Cambrian Mayan deposits. ...
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Journal Article
Published: 01 July 2023
Russ. Geol. Geophys. (2023) 64 (7): 839–846.
... Formation) stages of the middle Cambrian; 2) regional Kuonamka horizon, which is composed of Toyonian and Amgian deposits and occurs along the margins of the Siberian Platform; it is represented by the Inikan and Kuonamka formations in the east of the Siberian Platform and by the Paidugina Formation...
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Journal Article
Published: 01 January 2024
Russ. Geol. Geophys. (2024) 65 (1): 35–49.
...Fig. 9. Seismic time section along the composite profile 080314+080316 (Khandygskaya prospect). Indices of seismic reflectors: Rlh – base of the Lakhanda Group, Rnr – top of the Neryuen Formation, Rig – top of the Ignikan Formation, VR –base of the Vendian, K 2 – base of the Inikan Formation...
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Journal Article
Published: 01 February 2025
Russ. Geol. Geophys. (2025) 66 (2): 188–195.
... similarity to those of the bitumen of the underlying Inikan high-carbon formation – the famous Kuonamka complex of the Siberian Platform [ Kashirtsev, 2003 ; Kashirtsev et al., 2004 ]. Fig. 1. Location of wells in the Lena–Amga interfluve. 1 – support wells; 2 – hydrogeological wells; 3...
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