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Olenek Uplift

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Journal Article
Published: 01 July 2022
Journal of Paleontology (2022) 96 (4): 791–802.
... independently in different lineages in the late Ediacaran and early Cambrian. Herein we describe a new taxon, Ilankirus kessyusensis new genus new species, from the base of the Cambrian Stage 2 of the Olenek Uplift (Siberian Platform). These fossils occur as ornamented steinkerns in the shape of trilateral...
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Series: AAPG Studies in Geology
Published: 01 January 2013
DOI: 10.1306/13371591St643560
EISBN: 9781629812649
... updated from Khalimov et al. (1984). Different classes of permeability among sandstones (n = 300 samples) and siltstones (n = 40 samples) of the northern Olenek uplift.* Table 3. Different classes...
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Journal Article
Published: 01 September 2002
Russ. Geol. Geophys. (2002) 43 (9): 826–836.
.... This work was supported by grants from RFBR (01-05-64819 and 01-05-65057) and UIGGM (VMTK 1760). REFERENCES 1. Kaban’kov , V.Ya. , New data on stratigraphy of Lower- and Middle-Cambrian deposits of Olenek Uplift (lower reaches of Olenek River...
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Journal Article
Published: 01 June 1999
Russ. Geol. Geophys. (1999) 40 (6): 807–817.
...M. S. Yakshin One of the Riphean reference sections in Russia is located on the Olenek Uplift in the north of the Siberian Platform. This section is rich in stromatolites and is characterized by abundance of glauconite in almost all terrigenous deposits from bottom to top. This permitted...
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Journal Article
Published: 01 October 1998
Russ. Geol. Geophys. (1998) 39 (10): 1378–1392.
...I. V. Korovnikov A succession of trilobite assemblages has been revealed by examination of collections from the Lower Cambrian section on the Khorbosuonka River (Olenek Uplift). A stratigraphic subdivision scheme for the range under consideration was compiled on the basis of the recognized...
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Geographic location of the study area within the Olenek Uplift (a) and on the sketch map of Eurasia (b), and stratigraphic position of the studied fossils in the Kessyusa Group (c). U–Pb ages are from: 1 – Vishnevskaya et al., 2017; 2 – Bowring et al., 1993; 3 – Kaufman et al., 2012. Legend: 1 – sandstone; 2 – alternating sandstone and siltstone; 3 – limestone; 4 – dolostone; 5 – stratiform breccia of the Tas-Yuryakh volcanic complex; 6 – siltstone and mudstone; 7 – sandy and silty limestone; 8 – unconformity; 9–14 – first occurrence of key fossils after (Grazhdankin et al., 2020): 9 – Cambrotubulus decurvatus; 10 – Anabarites trisulcatus; 11 – Anabarites korobovi; 12 – Aldanella attleborensis; 13 – Watsonella crosbyi; 14 – Treptichnus pedum.
Published: 01 October 2023
Fig. 1. Geographic location of the study area within the Olenek Uplift ( a ) and on the sketch map of Eurasia ( b ), and stratigraphic position of the studied fossils in the Kessyusa Group ( c ). U–Pb ages are from: 1 – Vishnevskaya et al., 2017 ; 2 – Bowring et al., 1993 ; 3 – Kaufman et al
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Schematic map of Suhana sedimentary basin. OLUP, Olenek uplift; KTG, Kyutyungde graben; KDUP, Kuoika–Daldyn uplift; MNUP, Muna uplift; UDUP, Udzha uplift. Natural bitumen fields: 1, Olenekskoe; 2, Tsentral’no-Olenekskoe; 3, Vostochno-Anabarskoe; 4, Siligir-Markh-inskoe; 5, Udachnaya pipe, 6, Verkhnemunskoe. Hydrocarbon source rocks outcrops: 7, Khatyspyt Formation (Vendian) on the Khorbusuonka River; 8, Kuonamka Formation (lower–middle Cambrian) on the tributaries of Olenek River; 9, Kuonamka Formation, the southern and eastern slopes of the Anabar Shield; 10, Kuonamka Formation, Molodo River; 11, Kuonamka Formation, Muna and Kulenke Rivers.
Published: 01 October 2019
Fig. 1. Schematic map of Suhana sedimentary basin. OLUP, Olenek uplift; KTG, Kyutyungde graben; KDUP, Kuoika–Daldyn uplift; MNUP, Muna uplift; UDUP, Udzha uplift. Natural bitumen fields: 1, Olenekskoe; 2, Tsentral’no-Olenekskoe; 3, Vostochno-Anabarskoe; 4, Siligir-Markh-inskoe; 5, Udachnaya pipe
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Outcrop of the Khatyspyt Formation on the Khorbusuonka River (Olenek uplift).
Published: 01 October 2019
Fig. 7. Outcrop of the Khatyspyt Formation on the Khorbusuonka River (Olenek uplift).
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Schematic geologic structure of the Olenek uplift of the basement of the Siberian craton, after Gladkochub et al. (2016), modified. 1, Phanerozoic sedimentary cover; 2, Khorbusuonka Group (Ediacaran); 3, united Arymass, Debengda, and Khaipakh Formations (Meso–Neoproterozoic); 4, united Sygynakhtakh and Kyutyungde Formations (Mesoproterozoic); 5, dolerite sill (Mesoproterozoic); 6, granitoids of the Olenek complex (Paleoproterozoic); 7, metasedimentary rocks of the Eekit Formation (Paleoproterozoic); 8, faults; 9, sampling localities.
Published: 01 March 2018
Fig. 3. Schematic geologic structure of the Olenek uplift of the basement of the Siberian craton, after Gladkochub et al. (2016) , modified. 1 , Phanerozoic sedimentary cover; 2 , Khorbusuonka Group (Ediacaran); 3 , united Arymass, Debengda, and Khaipakh Formations (Meso–Neoproterozoic); 4
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Geological scheme of the Olenek uplift of the Siberian craton basement. 1, Phanerozoic sedimentary cover; 2, Khorbusuonka Group (Ediacaran); 3, united Arymas, Debengde, and Khaipakh Formations (Meso-Neoproterozoic); 4, united Sygynakhtakh and Kyutingde Formations (Mesoproterozoic); 5, dolerite sill (Mesoproterozoic); 6, basement (granitoids, metasedimentary rocks) (Paleoproterozoic); 7, faults; 8, sampling localities (K, Kyutingde River; S, Sololi River). Inset shows the location of the study area.
Published: 01 May 2016
Fig. 1. Geological scheme of the Olenek uplift of the Siberian craton basement. 1 , Phanerozoic sedimentary cover; 2 , Khorbusuonka Group (Ediacaran); 3 , united Arymas, Debengde, and Khaipakh Formations (Meso-Neoproterozoic); 4 , united Sygynakhtakh and Kyutingde Formations (Mesoproterozoic
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Stratigraphic sequence of Proterozoic deposits in the Olenek uplift of the Siberian craton basement. 1, conglomerates; 2, gravelstones; 3, sandstones; 4, siltstones; 5, mudstones; 6, carbonaceous-rock marks; 7, tuffaceous sediments; 8, limestones, silty limestones, and alternating limestones and siltstones; 9, dolomites, silty dolomites, and alternating dolomites and siltstones; 10, limestones and stromatolitic dolomites; 11, red-colored deposits; 12, syngenetic silicification; 13, dolerites; 14, granitoids; 15, metasedimentary rocks; 16, discordance.
Published: 01 May 2016
Fig. 2. Stratigraphic sequence of Proterozoic deposits in the Olenek uplift of the Siberian craton basement. 1 , conglomerates; 2 , gravelstones; 3 , sandstones; 4 , siltstones; 5 , mudstones; 6 , carbonaceous-rock marks; 7 , tuffaceous sediments; 8 , limestones, silty limestones
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Schematic map of the northwestern slope of Olenek Uplift (the Khorbusuonka and Kersyuke Rivers), with position of the studied sections. The outcrop of tuff breccia of the Tas-Yuryakh Volcanic Complex (Khorbusuonka River, Section 0910) which yielded the U-Pb zircon date of 543.9 ± 0.24 Ma (Bowring et al., 1993). Dash line contours a large block of the Turkut rocks. Continuous lines indicate boundaries of the diatreme. Scale bar: 10 m.
Published: 01 April 2015
Fig. 1. Schematic map of the northwestern slope of Olenek Uplift (the Khorbusuonka and Kersyuke Rivers), with position of the studied sections. The outcrop of tuff breccia of the Tas-Yuryakh Volcanic Complex (Khorbusuonka River, Section 0910) which yielded the U-Pb zircon date of 543.9 ± 0.24 Ma
Image
Schematic profile across the Olenek uplift and Bulkur anticline of the Verkhoyansk foredeep. 1, algal dolomites; 2, limestones; 3, clayey limestone; 4, mudstones and siltstones; 5, conglomerates and sandstones; 6, faults; 7, bitumen pools and bitumen occurrences; 8, calcite veins with bitumen.
Published: 01 January 2010
Fig. 6. Schematic profile across the Olenek uplift and Bulkur anticline of the Verkhoyansk foredeep. 1, algal dolomites; 2, limestones; 3, clayey limestone; 4, mudstones and siltstones; 5, conglomerates and sandstones; 6, faults; 7, bitumen pools and bitumen occurrences; 8, calcite veins
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Chemostratigraphic dating of Vendian deposits of the Olenek uplift. 1 — Lower Proterozoic folded basement (Eekit series); 2 — conglomerates and gravelstone; 3 — sandstones; 4 — mudstones and siltstones; 5 — variegated marls; 6 — dark bituminous limestones; 7 — dolomites. Carbon isotope composition for: 8 — limestones (a, unaltered and b, crystallized); 9 — dolomites (a, unaltered and b, crystallized); 10 — plus, minus, and average (A) isotope intervals. Inset shows the study area.
Published: 01 July 2004
Fig. 1. Chemostratigraphic dating of Vendian deposits of the Olenek uplift. 1 — Lower Proterozoic folded basement (Eekit series); 2 — conglomerates and gravelstone; 3 — sandstones; 4 — mudstones and siltstones; 5 — variegated marls; 6 — dark bituminous limestones; 7 — dolomites
Journal Article
Published: 08 November 2019
Geological Magazine (2020) 157 (1): 22–34.
... to the idea of the ‘Cambrian Explosion’ of animals and protists when the entire Earth system shifted rapidly into Phanerozoic mode. We conducted a multidisciplinary study of an informal ‘synstratotype’ of the lower Tommotian boundary in the upper Mattaia Formation, Kessyusa Group in the Olenek Uplift, NE...
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Journal Article
Published: 01 March 2018
Russ. Geol. Geophys. (2018) 59 (3): 226–237.
...Fig. 3. Schematic geologic structure of the Olenek uplift of the basement of the Siberian craton, after Gladkochub et al. (2016) , modified. 1 , Phanerozoic sedimentary cover; 2 , Khorbusuonka Group (Ediacaran); 3 , united Arymass, Debengda, and Khaipakh Formations (Meso–Neoproterozoic); 4...
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Simplified map of the Siberian Platform (left) showing Tommotian palaeogeography and principal facies distribution, modified after Khomentovsky & Karlova (2002), with additions from Grazhdankin et al. (2015). Sections that are relevant to the discussion of the Tommotian chemostratigraphy are located in the SE of the platform (1, Aldan River), on the Igarka Uplift (2, Sukharikha River), on the Anabar Uplift (3, Kotui and Kotuikan rivers) and on the Olenek Uplift (4, Olenek and Khorbusuonka rivers). Studied area of the northwestern slope of the Olenek Uplift (right), showing locations of the sections most informative for lower Tommotian chemostratigraphy.
Published: 08 November 2019
chemostratigraphy are located in the SE of the platform (1, Aldan River), on the Igarka Uplift (2, Sukharikha River), on the Anabar Uplift (3, Kotui and Kotuikan rivers) and on the Olenek Uplift (4, Olenek and Khorbusuonka rivers). Studied area of the northwestern slope of the Olenek Uplift (right), showing
Journal Article
Published: 01 October 2023
Russ. Geol. Geophys. (2023) 64 (10): 1179–1195.
...Fig. 1. Geographic location of the study area within the Olenek Uplift ( a ) and on the sketch map of Eurasia ( b ), and stratigraphic position of the studied fossils in the Kessyusa Group ( c ). U–Pb ages are from: 1 – Vishnevskaya et al., 2017 ; 2 – Bowring et al., 1993 ; 3 – Kaufman et al...
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Journal Article
Journal: GSA Bulletin
Published: 01 August 1996
GSA Bulletin (1996) 108 (8): 992–1003.
...Shane M. Pelechaty; Alan J. Kaufman; John P. Grotzinger Abstract Integrated sedimentologic, stratigraphic, and geochemical (δ 13 C, δ 18 O, Fe, Mn, and Sr) data from Vendian-Cambrian carbonate-ramp deposits of the northeast Siberian platform (Olenek uplift and Kharaulakh Mountains region) are used...
Journal Article
Published: 01 June 2023
Russ. Geol. Geophys. (2023) 64 (6): 724–734.
... 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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