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Kharaulakh Anticlinorium

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Journal Article

ORGANIC GEOCHEMISTRY OF ROCKS OF THE MIDDLE MEMBER OF THE VENDIAN KHARAYUTEKH FORMATION (Chekurovka Anticline, northeastern framing of the Siberian Platform) Available to Purchase

D.S. Melnik, T.M. Parfenova
Published: 01 March 2025
Russ. Geol. Geophys. (2025) 66 (3): 346–361.
DOI: https://doi.org/10.2113/RGG20244794
...D.S. Melnik; T.M. Parfenova The results of a geochemical study of rocks and dispersed organic matter (OM) of the middle member of the Vendian Kharayutekh Formation of the Chekurovka Anticline (Kharaulakh anticlinorium of the Verkhoyansk fold-and-thrust belt) close to the Siberian Platform border...
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View PDF for article title, ORGANIC GEOCHEMISTRY OF ROCKS OF THE MIDDLE MEMBER OF THE VENDIAN KHARAYUTEKH FORMATION (Chekurovka Anticline, northeastern framing of the Siberian Platform)
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Journal Article

The Early Cambrian bimodal magmatism in the northeastern Siberian Craton Available to Purchase

A.V. Prokopiev, A.K. Khudoley, O.V. Koroleva, G.G. Kazakova, D.K. Lokhov, S.V. Malyshev, A.I. Zaitsev, S.P. Roev, S.A. Sergeev, N.G. Berezhnaya, D.A. Vasiliev
Published: 01 January 2016
Russ. Geol. Geophys. (2016) 57 (1): 155–175.
DOI: https://doi.org/10.1016/j.rgg.2016.01.011
... of the northeastern Siberian Craton (Kharaulakh anticlinorium, contact between the Siberian Platform and the West Verkhoyansk sector of the Verkhoyansk fold-and-thrust belt united into an Early Cambrian bimodal complex. This complex comprises trachyrhyolites forming pebbles in conglomerates near the base...
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Sedimentary structures of the Lower Carboniferous rocks from the northern part of the Kharaulakh anticlinorium. a, Sandy turbidites of the Krestyakh Formation; graded bedding and submarine channels filled in with coarse clastic material; b, fine-grained turbidites with rare sandstone layers from the Tiksi Formation.

Sedimentary structures of the Lower Carboniferous rocks from the northern p... Available to Purchase

Published: 01 October 2013
Fig. 4. Sedimentary structures of the Lower Carboniferous rocks from the northern part of the Kharaulakh anticlinorium. a , Sandy turbidites of the Krestyakh Formation; graded bedding and submarine channels filled in with coarse clastic material; b , fine-grained turbidites with rare sandstone
Image
Composite m/z 85 and 127 mass-chromatograms of aliphatic hydrocarbon fractions of bitumens from Devonian, Carboniferous, and Permian mudstones of the Kharaulakh anticlinorium. 15–33, n-alkanes; Pr, pristane; Ph, phytane; 2,4-Dma, 2,4-dimethylalkanes; 2,7-Dma, 2,7-dimethylalkanes.

Composite m / z 85 and 127 mass-chromatograms of aliphatic hydrocarbon fr... Available to Purchase

Published: 01 August 2018
Fig. 2. Composite m / z 85 and 127 mass-chromatograms of aliphatic hydrocarbon fractions of bitumens from Devonian, Carboniferous, and Permian mudstones of the Kharaulakh anticlinorium. 15–33, n -alkanes; Pr, pristane; Ph, phytane; 2,4-Dma, 2,4-dimethylalkanes; 2,7-Dma, 2,7-dimethylalkanes.
Image
Total ion current mass-chromatograms of the aliphatic hydrocarbon fraction of bitumen from Carboniferous deposits of the Kharaulakh anticlinorium. Mass-fragmentograms m/z 69, 83 and mass spectra of alkene-3 and alkylcyclohexane C21. Bottom: the mass-spectrum and structure of squalene (peak S) in the TIC chromatogram.

Total ion current mass-chromatograms of the aliphatic hydrocarbon fraction ... Available to Purchase

Published: 01 August 2018
Fig. 3. Total ion current mass-chromatograms of the aliphatic hydrocarbon fraction of bitumen from Carboniferous deposits of the Kharaulakh anticlinorium. Mass-fragmentograms m/z 69, 83 and mass spectra of alkene-3 and alkylcyclohexane C 21 . Bottom: the mass-spectrum and structure of squalene
Image
Mass-chromatograms of aromatic bitumen fractions from (A) Carboniferous deposits of the Kharaulakh anticlinorium and (B) Cretaceous deposits of the Lena–Anabar basin. Mass-spectra of 17-desmethyl, 23-methylaromatic steroid C27. MPh, Methylphenanthrenes; DMPh, dimethylphenanthrenes; P, pyrene; R, retene; TTHPh, 1,1,7,8-tetramethyl-, 2,3,4-tetrahydrophenanthrene.

Mass-chromatograms of aromatic bitumen fractions from ( A ) Carboniferous d... Available to Purchase

Published: 01 August 2018
Fig. 4. Mass-chromatograms of aromatic bitumen fractions from ( A ) Carboniferous deposits of the Kharaulakh anticlinorium and ( B ) Cretaceous deposits of the Lena–Anabar basin. Mass-spectra of 17-desmethyl, 23-methylaromatic steroid C 27 . MPh, Methylphenanthrenes; DMPh, dimethylphenanthrenes
Image
Schematic geological map of the northern part of the front of the Verkhoyansk fold-and-thrust belt (the north of the Kharaulakh anticlinorium) (Prokopiev and Deikunenko, 2001), with modifications and supplement. The location of the mapped area is shown in Fig. 1. Deposits: 1, Cenozoic; 2, Cretaceous; 3, Triassic and Jurassic; 4, Permian; 5, Carboniferous; 6, Upper Precambrian and Cambrian; 7, thrusts; 8, other faults; 9, location of the studied sections and sampling localities.

Schematic geological map of the northern part of the front of the Verkhoyan... Available to Purchase

Published: 01 January 2016
Fig. 2. Schematic geological map of the northern part of the front of the Verkhoyansk fold-and-thrust belt (the north of the Kharaulakh anticlinorium) ( Prokopiev and Deikunenko, 2001 ), with modifications and supplement. The location of the mapped area is shown in Fig. 1 . Deposits: 1
Image
Composite stratigraphic sections of the Lower Carboniferous rocks of the Kharaulakh anticlinorium showing stratigraphic setting of the studied samples (after Abramov and Grigorieva, 1986; Ershova et al., 2013), modified). Sections: a, Krest-Tumsa; b, Tiksi; c, Taba-Bastakh, 1, mudstone; 2, siltstone; 3, sandstone; 4, gravely conglomerate; 5, pebbly conglomerate; 6, limestone; 7, dolomite; 8, chert; 9, sampling sites.

Composite stratigraphic sections of the Lower Carboniferous rocks of the Kh... Available to Purchase

Published: 01 October 2013
Fig. 3. Composite stratigraphic sections of the Lower Carboniferous rocks of the Kharaulakh anticlinorium showing stratigraphic setting of the studied samples (after Abramov and Grigorieva, 1986 ; Ershova et al., 2013 ), modified). Sections: a , Krest-Tumsa; b , Tiksi; c , Taba-Bastakh, 1
Journal Article

Hydrocarbons occluded by asphaltenes Available to Purchase

V.A. Kashirtsev
Published: 01 August 2018
Russ. Geol. Geophys. (2018) 59 (8): 975–982.
DOI: https://doi.org/10.1016/j.rgg.2018.07.017
...Fig. 2. Composite m / z 85 and 127 mass-chromatograms of aliphatic hydrocarbon fractions of bitumens from Devonian, Carboniferous, and Permian mudstones of the Kharaulakh anticlinorium. 15–33, n -alkanes; Pr, pristane; Ph, phytane; 2,4-Dma, 2,4-dimethylalkanes; 2,7-Dma, 2,7-dimethylalkanes. ...
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Age distribution diagrams of detrital zircons and igneous rocks. a, b, Histograms and age distribution probability curves of detrital zircons from Carboniferous rocks in the northern part of the Kharaulakh anticlinorium. Figures show approximate ages of peaks combined at least 3 measurements. c–g, Age distribution probability curves of zircons from igneous rocks and detrital zircons from volcanogenic-sedimentary rocks based on the data for: c, Central Taimyr (Pease et al., 2001; Vernikovskaya et al., 2004; Vernikovsky, 1996; Vernikovsky and Vernikovskaya, 2001; Zakharov et al., 1993); d, Taimyr–Severnaya Zemlya fold belt, southern part of the Kara terrane (north of Taimyr peninsula) (Pease and Scott, 2009; detrital zircons); e, Taimyr–Severnaya Zemlya fold belt, southern part of the Kara terrane (Bol’shevik and October Revolution Islands, Severnaya Zemlya archipelago) (Kaplan et al., 2001; Lorenz et al., 2007); f, Central Asian fold belt (Yenisei Ridge) (Vernikovskaya et al., 2002b, 2004, 2006, 2007, 2010; Vernikovsky et al., 2007, 2008); g, Central Asian fold belt (northern part of the Altai–Sayan area) (De Grave et al., 2009; Dobretsov and Buslov, 2007; Glorie et al., 2011; Kruk et al., 2011; Prokopiev et al., 2008 and its references; Rudnev, 2013; Rudnev et al., 2004). N, Number of dated grains.

Age distribution diagrams of detrital zircons and igneous rocks. a , b , ... Available to Purchase

Published: 01 October 2013
Fig. 5. Age distribution diagrams of detrital zircons and igneous rocks. a , b , Histograms and age distribution probability curves of detrital zircons from Carboniferous rocks in the northern part of the Kharaulakh anticlinorium. Figures show approximate ages of peaks combined at least 3
Image
Scheme of tectonic elements of structure-formational complex on the Siberian Platform. 1 – high-rank tectonic elements; 2 – major structures; 3 – outlines of the present-day occurrence of Middle Paleozoic deposits; 4 – structure-forming disjunctions; 5 – dike belts. Tectonic elements: I – Patom-Vilyui rift system (1 – Ygyatta trough, 2 – Suntar uplift, 3 – Kempendyai trough, 4 – Arbai-Sin’ uplift zone, 5 – Sarsan trough, 6, 7 – Tyukyan-Chybyda transverse uplift zone (6 – Chybyda uplift, 7 – Tyukyan uplift), 8 – Syangda trough, 9 – Loglor uplift, 10 – Linden trough, 11 – Khapchagai uplift, 12 – Tangnaryn trough, 13 – Vilyui-Markha dike belt, 14 – CharaSin’ dike belt); II – cis-Verkhoyansk marginal trough (15 – Sobopol’ graben, 16 – Kyutyungde-Dzhardzhan graben); III – West Verkhoyansk megaanticlinorium (17 – Sette-Daban horst-synclinorium, 18 – Kharaulakh anticlinorium); IV – Lena-Anabar trough (19 – Bilir-Udzha graben zone); V – Yenisei-Khatanga trough (20 – Balakhnya megabar, 21 – Rassokha megabar, 22 – Yangoda-Gorbita uplift, 23 – Taimyr uplift, 24 – Tanam-Malaya Kheta megabar); VI – Tunguska syneclise (25 – Putorana uplift, 26 – Voevodikha uplift, 27 – Tura trough, 28 – Kureika-Kheta trough, 29 – Khantai-Rybnaya megabar, 30 – Taishet-Rybnaya trough); VII – cis-Patom marginal trough.

Scheme of tectonic elements of structure-formational complex on the Siberia... Available to Purchase

Published: 01 April 2001
– Khapchagai uplift, 12 – Tangnaryn trough, 13 – Vilyui-Markha dike belt, 14 – CharaSin’ dike belt); II – cis-Verkhoyansk marginal trough (15 – Sobopol’ graben, 16 – Kyutyungde-Dzhardzhan graben); III – West Verkhoyansk megaanticlinorium (17 – Sette-Daban horst-synclinorium, 18 – Kharaulakh anticlinorium); IV
Journal Article

Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U–Pb dating of detrital zircons: role of erosion products of the Central Asian and Taimyr–Severnaya Zemlya fold belts Available to Purchase

A.V. Prokopiev, V.B. Ershova, E.L. Miller, A.K. Khudoley
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1195–1204.
DOI: https://doi.org/10.1016/j.rgg.2013.09.005
...Fig. 4. Sedimentary structures of the Lower Carboniferous rocks from the northern part of the Kharaulakh anticlinorium. a , Sandy turbidites of the Krestyakh Formation; graded bedding and submarine channels filled in with coarse clastic material; b , fine-grained turbidites with rare sandstone...
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View PDF for article title, Early Carboniferous paleogeography of the northern Verkhoyansk passive margin as derived from U–Pb dating of detrital zircons: role of erosion products of the Central Asian and Taimyr–Severnaya Zemlya fold belts
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Journal Article

Source rocks of Carboniferous–Lower Cretaceous terrigenous sediments of the northeastern Siberian Platform: results of Sm–Nd isotope–geochemical studies Available to Purchase

S.V. Malyshev, A.K. Khudoley, A.V. Prokopiev, V.B. Ershova, G.G. Kazakova, L.B. Terentyeva
Published: 01 March 2016
Russ. Geol. Geophys. (2016) 57 (3): 421–433.
DOI: https://doi.org/10.1016/j.rgg.2016.03.005
... groups of Carboniferous samples from the Kharaulakh area ( Table 1 , Figs. 6 , 8 a ) have different isotope characteristics. The northern part of the area is characterized by a wide range of ε Nd ( t ) values, whereas in the more southerly part of the Kharaulakh anticlinorium, which is farther from...
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View PDF for article title, Source rocks of Carboniferous–Lower Cretaceous terrigenous sediments of the northeastern Siberian Platform: results of Sm–Nd isotope–geochemical studies
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Journal Article

Sedimentology and isotope geochemistry of Riphean carbonates in the Kharaulakh Range of northern East Siberia Available to Purchase

E.M. Khabarov, O.P. Izokh
Published: 01 May 2014
Russ. Geol. Geophys. (2014) 55 (5-6): 629–648.
DOI: https://doi.org/10.1016/j.rgg.2014.05.008
...E.M. Khabarov; O.P. Izokh Abstract Stable carbon isotope variations in primarily offshore Proterozoic carbonates of the Eselekh, Neleger, and Sietachan Formations in the Kharaulakh Range of northern East Siberia provide important information on the depositional history of the Riphean complexes...
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View PDF for article title, Sedimentology and isotope geochemistry of Riphean carbonates in the <span class="search-highlight">Kharaulakh</span> Range of northern East Siberia
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Journal Article

The Origin of Paleozoic Terranes in Northeastern Asia: Geologic Evidence for Rifting of the Pericratonic Margin of the Siberian Paleocontinent and for Migration of Its Fragments Available to Purchase

A.V. Kanygin, T.V. Gonta, A.V. Timokhin
Published: 01 November 2020
Russ. Geol. Geophys. (2020) 61 (11): 1197–1211.
DOI: https://doi.org/10.15372/RGG2019140
... representation of the fold geometry, they compiled structural profiles and reconstructed down-plunge projections for nine intersections within the West Verkhoyansk foldbelt, which is subdivided into the Kharaulakh, Orulgan, Kuranakh, and Barain segments, differing in structural features. This paper...
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Map of cratons and orogenic belts of Northeast Asia (after Parfenov et al., 2003, modified). 1–5, cratons: 1, ancient platform; 2, shields and uplifts of the crystalline basement of the Siberian platform (An, Anabar shield; AS, Aldan–Stanovoi shield; Ol, Olenek uplift; UL, Ust’-Lena uplift); 3, subsided craton margin, fold-and-thrust belt (ST, South Taimyr; EA, East Angara; BP, Baikal–Patom; VR, Verkhoyansk); 4, Meso- and Neoproterozoic rifts; 5, Middle Paleozoic rifts; 6–13, orogenic belts of variable age: 6, Circum-Siberia (CS), Neoproterozoic; 7, Yenisei–Transbaikalian (YT), Late Cambrian–Early Ordovician; 8, Altai (AL), Silurian; 9, South Mongolia–Khingan (AM), West Siberian (WS), and Taimyr–Severnaya Zemlya (TS), Late Paleozoic; 10, Mongol–Okhotsk (MO), Late Paleozoic–Early Mesozoic; 11, Chukotka (CH), Middle–Late Jurassic; 12, Verkhoyansk–Kolyma (VK), South Anyui (SA), and Honshu–Sikhote-Alin (HS), Late Jurassic–Early Cretaceous; 13, Kolyma–Omolon superterrane (KM); 14, cratonal terranes: OH, Okhotsk; KOM, Omolon; 15, fragments of Neoproterozoic orogenic belts: TM, Tuva–Mongolia terrane and AR, Argun terrane; 16, fragments of Early Paleozoic orogenic belts: BJ, Bureya–Jiamusi terrane and KAR, Kara terrane; 17, oceanic crust; 18, thrust; 19, strike-slip fault; 20, other faults; 21, anticlinorium (Kh, Kharaulakh; O, Orulgan; K, Kuranakh; B, Baraya); 22, synclinorium (S, South Verkhoyansk). Rectangle indicates the study area.

Map of cratons and orogenic belts of Northeast Asia (after Parfenov et al.... Available to Purchase

Published: 01 October 2013
orogenic belts: BJ, Bureya–Jiamusi terrane and KAR, Kara terrane; 17 , oceanic crust; 18 , thrust; 19 , strike-slip fault; 20 , other faults; 21 , anticlinorium (Kh, Kharaulakh; O, Orulgan; K, Kuranakh; B, Baraya); 22 , synclinorium (S, South Verkhoyansk). Rectangle indicates the study area.
Journal Article

HALMEIC FORMATIONS AND PETROLEUM POTENTIAL OF PALEOZOIC RESERVOIRS OF THE SIBERIAN PLATFORM Available to Purchase

G. S. Fradkin
Published: 01 April 2001
Russ. Geol. Geophys. (2001) 42 (4): 573–584.
... – Khapchagai uplift, 12 – Tangnaryn trough, 13 – Vilyui-Markha dike belt, 14 – CharaSin’ dike belt); II – cis-Verkhoyansk marginal trough (15 – Sobopol’ graben, 16 – Kyutyungde-Dzhardzhan graben); III – West Verkhoyansk megaanticlinorium (17 – Sette-Daban horst-synclinorium, 18 – Kharaulakh anticlinorium); IV...
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The Triassic of New Siberian Islands Archipelago and Its Position in the Structure of Sedimentary Cover of the Laptev Sea Shelf Available to Purchase

B.L. Nikitenko, V.P. Devyatov, A.G. Konstantinov, E.S. Sobolev, A.V. Yadrenkin, E.B. Pestchevitskaya, N.K. Lebedeva, A.A. Goryacheva
Published: 01 April 2022
Russ. Geol. Geophys. (2022) 63 (4): 383–397.
DOI: https://doi.org/10.2113/RGG20214421
... in the structure of the sedimentary levels of this area. However, the section yields a complete set of zonal ammonoid and bivalve species in areas adjacent to the Verkhoyansk mega-anticlinorium ( Koren’ and Kotlyar, 2009 ). Fig. 6. Stratigraphic scheme of the Triassic of Kotelny Island...
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Journal Article

TRIASSIC DIAMOND PLACERS ON THE NORTHEASTERN SIBERIAN PLATFORM Available to Purchase

S.A. Grakhanov, V.I. Koptil’
Published: 01 November 2003
Russ. Geol. Geophys. (2003) 44 (11): 1189–1199.
... Peninsula. South of the Kharaulakh anticlinorium no special search for diamonds was carried out but they were found in the alluvium of the Uel’-Siktyakh River, a right tributary of the Lena River, which erodes the Carnian sediments. Fig. 1. Schematic occurrence of diamondiferous sites of Triassic...
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Integrated chronostratigraphy of the Vendian System of Siberia: implications for a global stratigraphy Available to Purchase

SHANE M. PELECHATY
Published: 01 December 1998
Journal of the Geological Society (1998) 155 (6): 957–973.
DOI: https://doi.org/10.1144/gsjgs.155.6.0957
... Journal of Geology 1996b 104 543 564 Pelechaty S.M. Kaufman A.J. Grotzinger J.P. Evaluation of δ 13 C isotope stratigraphy for intrabasinal correlation: Vendian strata of the Olenek uplift and Kharaulakh Mountains, Siberian platform, Russia Geological Society of America Bulletin...
View PDF for article title, Integrated chronostratigraphy of the Vendian System of Siberia: implications for a global stratigraphy
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