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Goloustnaya Formation

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Lithology and correlation of the Goloustnaya Formation sections, western Cisbaikalia (Kurtun and Bugul’deika Rivers), and stratigraphic position of the studied samples. Numeral above the column is the exposure number (see Fig. 1). 1–3 — limestones: 1 — stromatolitic, from columnar (a) and sheet (algal laminites) (b) stromatolites, 2 — oolite-pelloid-pisolitic (a) and pelloid-intraclastic (b), 3 — partly recrystallized siltite-micritic (a) and argillaceous (b); 4–6 — dolomites: 4 — stromatolitic, from columnar (a) and sheet (algal laminites) (b) stromatolites, 5 — oolite-pelloid-pisolitic (a) and pelloid-intraclastic (b), 6 — recrystallized micritesiltitic (a) and sandy (b); 7 — coarse-pebble conglomerates; 8 — sandstones; 9 — siltstones; 10 — clay-silty shales; 11 — mudstones and clay shales; 12 — predominantly volcanoclastic rocks; 13 — large gaps.

Lithology and correlation of the Goloustnaya Formation sections, western Ci... Available to Purchase

Published: 01 October 2005
Fig. 2. Lithology and correlation of the Goloustnaya Formation sections, western Cisbaikalia (Kurtun and Bugul’deika Rivers), and stratigraphic position of the studied samples. Numeral above the column is the exposure number (see Fig. 1 ). 1–3 — limestones: 1 — stromatolitic, from columnar
Journal Article

Testing the snowball Earth hypothesis for the Ediacaran Available to Purchase

Alexei V. Ivanov, Anatoly M. Mazukabzov, Arkady M. Stanevich, Stanislav V. Palesskiy, Olga A. Kozmenko
Journal: Geology
Published: 01 July 2013
Geology (2013) 41 (7): 787–790.
DOI: https://doi.org/10.1130/G34345.1
...Alexei V. Ivanov; Anatoly M. Mazukabzov; Arkady M. Stanevich; Stanislav V. Palesskiy; Olga A. Kozmenko Abstract Ediacaran Siberia was at tropical paleolatitudes when the glacigenic strata of the Goloustnaya Formation (Baikal Group, Siberia) were deposited at sea level. The presence of such deposits...
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Distribution of (a) major typomorphic elements and (b) minor elements in carbonate deposits of the Goloustnaya and Uluntui Formations. Carbonate deposits: 1, Goloustnaya Formation (18 samples); 2, shallow deposits of the Uluntui Formation (11 samples); 3, relatively deep-water deposits of the Uluntui Formation (24 samples).

Distribution of ( a ) major typomorphic elements and ( b ) minor elements i... Available to Purchase

Published: 01 October 2013
Fig. 7. Distribution of ( a ) major typomorphic elements and ( b ) minor elements in carbonate deposits of the Goloustnaya and Uluntui Formations. Carbonate deposits: 1 , Goloustnaya Formation (18 samples); 2 , shallow deposits of the Uluntui Formation (11 samples); 3 , relatively deep-water
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REE pattern in terrigenous deposits of the Baikal Group and in the post-Archean Australian shale continental crust (PAAS). Designations: (a) 1, PAAS; 2–5, terrigenous deposits of the Goloustnaya Formation; (b) 1, PAAS; 2, 3, terrigenous deposits of the Kachergat Formation.

REE pattern in terrigenous deposits of the Baikal Group and in the post-Arc... Available to Purchase

Published: 01 October 2013
Fig. 6. REE pattern in terrigenous deposits of the Baikal Group and in the post-Archean Australian shale continental crust (PAAS). Designations: ( a ) 1 , PAAS; 2 – 5 , terrigenous deposits of the Goloustnaya Formation; ( b ) 1 , PAAS; 2 , 3 , terrigenous deposits of the Kachergat Formation.
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Provenance compositions for terrigenous deposits of the Baikal and Oselok Groups on the base of Taylor and McLennan’s chart. 1, Goloustnaya Formation of the Baikal Group; 2, Uluntui Formation of the Baikal Group; 3, Oselok Group. Composition fields: G, granites; S, sediments; B, basic rocks; UB, ultrabasic rocks.

Provenance compositions for terrigenous deposits of the Baikal and Oselok G... Available to Purchase

Published: 01 October 2013
Fig. 16. Provenance compositions for terrigenous deposits of the Baikal and Oselok Groups on the base of Taylor and McLennan’s chart. 1, Goloustnaya Formation of the Baikal Group; 2 , Uluntui Formation of the Baikal Group; 3 , Oselok Group. Composition fields: G, granites; S, sediments; B
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Deformation in stratotype area of Baikal Group (Western Baikal region). A — Location map of Baikal Group and structural sections; 1 — Quaternary rocks; 2 — Vendian Ushakovka Formation; 3–5 — Late Riphean Kachergat (3), Uluntui (4), and Goloustnaya (5) formations; 6 — Archean-Paleoproterozoic; 7 — Early Paleozoic collisional gabbroids; 8 — Paleoproterozoic granitoids of Primorsky complex; 9 — faults; 10 — sections. B–E — structural sections: B — left bank of Goloustnaya River, opposite B. Cheremshanka creek mouth; C, D — Ozerko valley, from detailed structural studies (Mazukabzov et al., 2001) (C) and from 1:50,000 geological surveys (D); E — Kutrun River valley, after our data (1–3 are insets of enlarged sections of selected sites); 11 — Quaternary deposits; 12–15 — Baikal Group: 12 — Kachergat Formation, 13 — Upper Uluntui subformation, 14 — lower Uluntui subformation, 15 — Goloustnaya Formation; 16 — Primorsky granitoids; 17 — faults; 18 — sampling sites for δ13C (Khabarov and Ponomarchuk, 2005).

Deformation in stratotype area of Baikal Group (Western Baikal region). A ... Available to Purchase

Published: 01 January 2007
Fig. 3. Deformation in stratotype area of Baikal Group (Western Baikal region). A — Location map of Baikal Group and structural sections; 1 — Quaternary rocks; 2 — Vendian Ushakovka Formation; 3–5 — Late Riphean Kachergat ( 3 ), Uluntui ( 4 ), and Goloustnaya ( 5 ) formations; 6
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U–Pb (<1 Ga) and Pb–Pb (>1 Ga) histograms and curves for the relative probability of the age of detrital zircon from the Neoproterozoic sedimentary rocks of the southern Siberian craton (modified after (Gladkochub et al., 2013)). a–c, Baikal Group: a, Goloustnaya Formation; b, Uluntui Formation; c, Kachergat Formation; d, Ushakovka Formation.

U–Pb (<1 Ga) and Pb–Pb (>1 Ga) histograms and curves for the relative... Available to Purchase

Published: 01 October 2013
Fig. 4. U–Pb (<1 Ga) and Pb–Pb (>1 Ga) histograms and curves for the relative probability of the age of detrital zircon from the Neoproterozoic sedimentary rocks of the southern Siberian craton (modified after ( Gladkochub et al., 2013 )). a – c , Baikal Group: a , Goloustnaya Formation
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Schematic geologic structure of the Nugan Brook basin, modified from Mazukabzov et al. (2018). 1–3, Baikal Group: 1, Kachergat Formation, 2, Uluntui Formation, 3, Goloustnaya Formation; 4, Nugan Formation; 5, Siberian Platform basement rocks; 6, faults; 7, sampling localities. Inset: 1–3, Siberian Platform: 1, Archean–Paleoproterozoic rocks (basement), 2, late Precambrian rocks, 3, early Paleozoic rocks; 4, Central Asian Orogenic Belt; 5, study area.

Schematic geologic structure of the Nugan Brook basin, modified from Mazuka... Available to Purchase

Published: 01 January 2023
Fig. 3. Schematic geologic structure of the Nugan Brook basin, modified from Mazukabzov et al. ( 2018 ). 1–3 , Baikal Group: 1 , Kachergat Formation, 2 , Uluntui Formation, 3 , Goloustnaya Formation; 4 , Nugan Formation; 5 , Siberian Platform basement rocks; 6 , faults; 7 , sampling
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Schematic geologic structure of the left bank of the Bugul’deika (Barlog mouth area). Compiled using Ryabykh’s Geological Map, scale 1 : 50,000 (1973), and our data. 1 — Quaternary deposits; 2, 3 — deposits of the Baikal Group (Riphean): 2 — Ulungui and 3 — Goloustnaya Formations; 4 — volcanic rocks of the Khotskaya Formation; 5 — granitoids of the Primorsky complex (Early Proterozoic); 6 — dislocations: a — thrusts, b — faults; 7 — structural elements: a — dip, b — granitoid fracturing; 8 — studied volcanic profiles and their numbers; 9 — localities of sampling for isotope dating.

Schematic geologic structure of the left bank of the Bugul’deika (Barlog mo... Available to Purchase

Published: 01 October 2008
Fig. 3. Schematic geologic structure of the left bank of the Bugul’deika (Barlog mouth area). Compiled using Ryabykh’s Geological Map, scale 1 : 50,000 (1973), and our data. 1 — Quaternary deposits; 2 , 3 — deposits of the Baikal Group (Riphean): 2 — Ulungui and 3 — Goloustnaya
Journal Article

The Vendian passive continental margin in the southern Siberian Craton: geochemical and isotopic (Sr, Sm–Nd) evidence and U–Pb dating of detrital zircons by the LA-ICP-MS method Available to Purchase

E.F. Letnikova, A.B. Kuznetsov, I.A. Vishnevskaya, S.V. Veshcheva, A.I. Proshenkin, H. Geng
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1177–1194.
DOI: https://doi.org/10.1016/j.rgg.2013.09.004
...Fig. 7. Distribution of ( a ) major typomorphic elements and ( b ) minor elements in carbonate deposits of the Goloustnaya and Uluntui Formations. Carbonate deposits: 1 , Goloustnaya Formation (18 samples); 2 , shallow deposits of the Uluntui Formation (11 samples); 3 , relatively deep-water...
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View PDF for article title, The Vendian passive continental margin in the southern Siberian Craton: geochemical and isotopic (Sr, Sm–Nd) evidence and U–Pb dating of detrital zircons by the LA-ICP-MS method
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Journal Article

CARBON ISOTOPES IN THE UPPER RIPHEAN DEPOSITS OF THE BAIKAL GROUP IN WESTERN CISBAIKALIA: STRATIGRAPHIC IMPLICATIONS Available to Purchase

E.M. Khabarov, V.A. Ponomarchuk
Published: 01 October 2005
Russ. Geol. Geophys. (2005) 46 (10): 1019–1037.
...Fig. 2. Lithology and correlation of the Goloustnaya Formation sections, western Cisbaikalia (Kurtun and Bugul’deika Rivers), and stratigraphic position of the studied samples. Numeral above the column is the exposure number (see Fig. 1 ). 1–3 — limestones: 1 — stromatolitic, from columnar...
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View PDF for article title, CARBON ISOTOPES IN THE UPPER RIPHEAN DEPOSITS OF THE BAIKAL GROUP IN WESTERN CISBAIKALIA: STRATIGRAPHIC IMPLICATIONS
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Journal Article

Early evolution of the Paleoasian ocean: LA-ICP-MS dating of detrital zircon from Late Precambrian sequences of the southern margin of the Siberian craton Available to Purchase

D.P. Gladkochub, A.M. Stanevich, A.M. Mazukabzov, T.V. Donskaya, S.A. Pisarevsky, G. Nicoll, Z.L. Motova, T.A. Kornilova
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1150–1163.
DOI: https://doi.org/10.1016/j.rgg.2013.09.002
...Fig. 4. U–Pb (<1 Ga) and Pb–Pb (>1 Ga) histograms and curves for the relative probability of the age of detrital zircon from the Neoproterozoic sedimentary rocks of the southern Siberian craton (modified after ( Gladkochub et al., 2013 )). a – c , Baikal Group: a , Goloustnaya Formation...
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View PDF for article title, Early evolution of the Paleoasian ocean: LA-ICP-MS dating of detrital zircon from Late Precambrian sequences of the southern margin of the Siberian craton
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Northern segment of the Paleoasian Ocean: Neoproterozoic deposition history and geodynamics Available to Purchase

A.M. Stanevich, A.M. Mazukabzov, A.A. Postnikov, V.K. Nemerov, S.A. Pisarevsky, D.P. Gladkochub, T.V. Donskaya, T.A. Kornilova
Published: 01 January 2007
Russ. Geol. Geophys. (2007) 48 (1): 46–60.
DOI: https://doi.org/10.1016/j.rgg.2006.12.005
...Fig. 3. Deformation in stratotype area of Baikal Group (Western Baikal region). A — Location map of Baikal Group and structural sections; 1 — Quaternary rocks; 2 — Vendian Ushakovka Formation; 3–5 — Late Riphean Kachergat ( 3 ), Uluntui ( 4 ), and Goloustnaya ( 5 ) formations; 6...
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View PDF for article title, Northern segment of the Paleoasian Ocean: Neoproterozoic deposition history and geodynamics
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Geological sketch map of the Goloustnaya–Kurtun River basins, with sampling sites (modified after (Gladkochub et al., 2013)). 1, Cenozoic sediments; 2, Vendian–Cambrian transitional rocks; 3–6, Neoproterozoic rocks: 3, Ushakovka Formation; 4–6, formations of the Baikal Group: 4, Kachergat; 5, Uluntui; 6, Goloustnaya; 7, Early Proterozoic granitoids (Primorsky complex); 8, metamorphic and igneous rocks of the Early Paleozoic Ol’khon terrane, Central Asian Fold Belt; 9, faults; 10, sampling sites and sample numbers.

Geological sketch map of the Goloustnaya–Kurtun River basins, with sampling... Available to Purchase

Published: 01 October 2013
Fig. 2. Geological sketch map of the Goloustnaya–Kurtun River basins, with sampling sites (modified after ( Gladkochub et al., 2013 )). 1 , Cenozoic sediments; 2 , Vendian–Cambrian transitional rocks; 3 – 6 , Neoproterozoic rocks: 3 , Ushakovka Formation; 4 – 6 , formations of the Baikal
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REE pattern in carbonate deposits of the Goloustnaya and Uluntui Formations. Designations follow Fig. 7.

REE pattern in carbonate deposits of the Goloustnaya and Uluntui Formations... Available to Purchase

Published: 01 October 2013
Fig. 8. REE pattern in carbonate deposits of the Goloustnaya and Uluntui Formations. Designations follow Fig. 7 .
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Stromatolites of Neoproterozoic of Baikal-Lena SFA. Formation: mr — Mariinsk, br — Barakun, kl — Kalancha, čn — Chencha, gl — Goloustnaya, ul — Uluntui, sn — Sen’, tr — Torgi. Stromatolite Parmites sp. — Ondok Formation of Olokit zone.

Stromatolites of Neoproterozoic of Baikal-Lena SFA. Formation: mr — Mariins... Available to Purchase

Published: 01 January 2008
Fig. 9. Stromatolites of Neoproterozoic of Baikal-Lena SFA. Formation: mr — Mariinsk, br — Barakun, kl — Kalancha, čn — Chencha, gl — Goloustnaya, ul — Uluntui, sn — Sen’, tr — Torgi. Stromatolite Parmites sp. — Ondok Formation of Olokit zone.
Journal Article

Stratigraphic Structure of the Vendian Oil and Gas Complex of the Southern Oil and Gas Regions of the Lena–Tunguska Province of the Siberian Platform Available to Purchase

N.V. Mel’nikov
Published: 01 January 2024
Russ. Geol. Geophys. (2024) 65 (1): 50–59.
DOI: https://doi.org/10.2113/RGG20234646
... Formation in different Baikalian colors is shown in Fig. 4 A , which depicts the well logs in the Irkutsk zone ( Fig. 4 ). In the northwestern logs, the Typta Formation lies on the Goloustnaya Formation in the Morozov well. In the section of the Bokhan well, the Typta Formation lies on the carbonates...
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View PDF for article title, Stratigraphic Structure of the Vendian Oil and Gas Complex of the Southern Oil and Gas Regions of the Lena–Tunguska Province of the Siberian Platform
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A — Major-element patterns in carbonaceous silty mudstones and siltstones of Goloustnaya (gl, n = 6), Uluntui (ul, n = 9), Kachergat (kcv1, n = 24; kcv2, n = 11) formations. B — REE patterns in carbonaceous silty mudstones and siltstones of Goloustnaya (gl, n = 28), Uluntui (ul, n = 189), Kachergat (kcv1, n = 255; kcv2, n = 175) formations. Analytical procedures carried out at Laboratory of East Siberian Research Institute for Geology, Geophysics, and Mineral Resources (Irkutsk). Whole-rock chemistry: analyst G.S. Katsnelson, Corg determination: analyst E.A. Razvozzhaeva, XRD (Ba, Sr, Zr, Th, U): analyst A.M. Kharchenko, quantitative spectrometry (Cu, Ni, Co, Cr, V, Mo, B): analyst I.S. Koroleva, major- and trace-element contents normalized against black shale standard SCHS-1 (Petrov et al., 2004).

A — Major-element patterns in carbonaceous silty mudstones and siltstones ... Available to Purchase

Published: 01 January 2007
Fig. 4. A — Major-element patterns in carbonaceous silty mudstones and siltstones of Goloustnaya (gl, n = 6), Uluntui (ul, n = 9), Kachergat ( kc v 1 , n = 24; kc v 2 , n = 11) formations. B — REE patterns in carbonaceous silty mudstones and siltstones
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a – Tectonic framework of the Siberian craton (Donskaya, 2020): 1 – Archean terranes; 2 – Paleoproterozoic terranes; 3 – Archean suture zones; 4–6 – orogenic belts and collisional zones of different ages: 2.00–1.95 Ga (4), 1.95–1.90 Ga (5), and 1.90–1.87 Ga (6); 7 – exposed basement inlier; 8 – contours of tectonic blocks assembled into the Akitkan orogen: T – Tonod, Ch – Chuya, S – Sarma, G – Goloustnaya.

a – Tectonic framework of the Siberian craton ( Donskaya, 2020 ): 1 – Ar... Available to Purchase

Published: 01 May 2024
sediments; 2 – early Paleozoic rocks of the Olkhon terrane of the Central Asian Orogenic Belt (CAOB); 3 – 5 – clastic and carbonate deposits of the Baikal Group, including the Kachergat ( 3 ), Uluntui ( 4 ), and Goloustnaya ( 5 ) formations; 6 – Nugan Formation clastic sediments; 7 – dolerite dikes
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Geological map of southern Siberian Craton, cross section (A-B) at Goloustnaya site, and generalized stratigraphic scheme for Ediacaran. Ages for Uluntui Formation and granites at basement are from Kuznetsov et al. (2013) and Mazukabzov et al. (2001), respectively. Inset is from Smith (2009).

Geological map of southern Siberian Craton, cross section (A-B) at Goloustn... Available to Purchase

Published: 01 July 2013
Figure 2. Geological map of southern Siberian Craton, cross section (A-B) at Goloustnaya site, and generalized stratigraphic scheme for Ediacaran. Ages for Uluntui Formation and granites at basement are from Kuznetsov et al. (2013) and Mazukabzov et al. (2001) , respectively. Inset is from