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Khapchagai Uplift

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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.
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
Published: 01 August 2014
Russ. Geol. Geophys. (2014) 55 (8): 1003–1008.
.... However, the development of the Mastakhskoe field had to be initiated because of a crisis in the gas supply of Yakutsk, so that the proposal of VNIPIGazdobycha to assess the commmercial significance of the oil rim in that field was not implemented. The Khapchagai megaswell is the largest uplifted...
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Zones of cleavage joints in producing beds on local uplifts (l.u.) of Khapchagai dome (Vilyui basin). 1 – wells without joints and their numbers; 2 – wells with joints and their numbers; 3 – hypothetical zone of joints; 4 – pinch-out of zones with paleoseismic joints; 5 – total thicknesses of zones of paleoseismic joints; 6 – depth contour lines of TP reflector; 7 – predicted seismic faults.
Published: 01 November 2001
Fig. 4. Zones of cleavage joints in producing beds on local uplifts (l.u.) of Khapchagai dome (Vilyui basin). 1 – wells without joints and their numbers; 2 – wells with joints and their numbers; 3 – hypothetical zone of joints; 4 – pinch-out of zones with paleoseismic joints; 5 – total
Journal Article
Published: 01 August 2018
Russ. Geol. Geophys. (2018) 59 (8): 975–982.
.... , Zhang , L. , Graciaa , A. , Creux , P. , 2012 . Experimental studies on the adsorption/occlusion phenomena inside the macromolecular structures of asphaltenes . Energy and Fuels 26 , 1746 – 1755 . The superdeep well SV-27 was drilled at the top of the Khapchagai uplift, Vilyui...
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Journal Article
Published: 01 August 2021
Russ. Geol. Geophys. (2021) 62 (08): 914–928.
...-condensate fields have been discovered in the basin and most of them are confined to two large positive structures, the Khapchagai megaswell and the Loglor swell ( Pogodayev and Sitnikov, 2008 ; Pogodayev et al., 2012 ; Pogodaev et al., 2015 ; Pogodaev, 2018 ). Overall, they span the stratigraphic...
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Journal Article
Published: 01 November 2001
Russ. Geol. Geophys. (2001) 42 (11): 1682–1690.
...Fig. 4. Zones of cleavage joints in producing beds on local uplifts (l.u.) of Khapchagai dome (Vilyui basin). 1 – wells without joints and their numbers; 2 – wells with joints and their numbers; 3 – hypothetical zone of joints; 4 – pinch-out of zones with paleoseismic joints; 5 – total...
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Geology of the middle Paleozoic structural level in the east of the Siberian Platform modified from (Gaiduk, 1988; Prokopiev et al., 2020). 1 – Famennian–lower Carboniferous tuff-sedimentary complex; 2 – Frasnian effusive complex; 3 – areas of inferred occurrence of basalt for the entire Upper Devonian–lower Carboniferous section; 4 – structural boundaries identified in Devonian–lower Carboniferous deposits (uplifts: Ar – Arbay, Us – Upper Sinsk, Lg – Loglor, Sn – Suntar, Kp – Khapchagai, Tk – Tyukyan, Chb – Chybyda; depressions: Km – Kempendyai, Ln – Linde, Sg – Syangda, Sr – Sarsan, Tn – Tangnaryn, Yg – Ygyatta; 5 – faults (A – Angara–Vilyui, B – Bappagai, U – Upper Sinsk, K – Kempendyai, N – Nyurba); 6 – boundary of Devonian–lower Carboniferous rocks; 7 – thickness (km) of Upper Devonian–lower Carboniferous deposits; 8 – exposed crystalline basement; 9 – middle Paleozoic dolerite dikes; 10 – Devonian gabbro-dolerite chonoliths; 11 – Devonian basalt pipes; 12 – location of sample MIR-12-51 from the dike in which melt inclusions were studied; 13–14 – ages (Ma) of middle Paleozoic dikes and basalts from (Polyansky et al., 2017 and references therein; Guzev et al., 2021): 13 – U–Pb (green spots), 14 – 40Ar/39Ar (black spots), red italics next to open spots show ages of dolerite sills from boreholes (Fig. 3, Suppl. Mat., Fig. S1).
Published: 01 July 2024
for the entire Upper Devonian–lower Carboniferous section; 4 – structural boundaries identified in Devonian–lower Carboniferous deposits (uplifts: Ar – Arbay, Us – Upper Sinsk, Lg – Loglor, Sn – Suntar, Kp – Khapchagai, Tk – Tyukyan, Chb – Chybyda; depressions: Km – Kempendyai, Ln – Linde, Sg – Syangda, Sr
Journal Article
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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Journal Article
Published: 01 August 1996
Russ. Geol. Geophys. (1996) 37 (8): 195–201.
... stage, Riphean, took about 700 Ma and was characterized by accumulation first of terrigenous and then chiefly carbonate sediments over the margins of the Siberian Craton and in separate troughs and depressions, between which denudation-subjected uplifts of considerable area were preserved...
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Journal Article
Published: 01 January 2004
Russ. Geol. Geophys. (2004) 45 (1): 121–126.
... hydrostatic pressure by 15–20 MPa; composition of this gas is distinguished from the gases of the Nepa-Botuobiya deposits in having more methane homologs; — prospecting surveys at the zone of junction of the Nyuya-Dzherba depression and the Suntar uplift, where the Suntar nonanticlinal trap is outlined...
Journal Article
Published: 01 November 2023
Russ. Geol. Geophys. (2023) 64 (11): 1267–1282.
.... Grazhdankin) 05 06 2023 20 10 2023 © 2023, Novosibirsk State University 2023 Novosibirsk State University The Upper Vendian sedimentary succession of the northeast of the Siberian Platform in sections along the northwestern slope of the Olenek uplift and in the Kharaulakh Ranges...
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Journal Article
Published: 01 July 2024
Russ. Geol. Geophys. (2024) 65 (7): 814–830.
... for the entire Upper Devonian–lower Carboniferous section; 4 – structural boundaries identified in Devonian–lower Carboniferous deposits (uplifts: Ar – Arbay, Us – Upper Sinsk, Lg – Loglor, Sn – Suntar, Kp – Khapchagai, Tk – Tyukyan, Chb – Chybyda; depressions: Km – Kempendyai, Ln – Linde, Sg – Syangda, Sr...
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Series: Investigations in Geophysics
Published: 01 January 2002
DOI: 10.1190/1.9781560802068.ch12
EISBN: 9781560802068
.... The northern and eastern edges of the depression and its central part are clearly seen in the map. We can confidently outline some large-scale tectonic elements within the depression: I = the Tarnog uplift, II = the Tot’ma sag, III = the Biryakov sag, IV = the Soligalich graben, V = the Roslyatin graben, VI...
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