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eastern Siberian Platform

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Journal Article
Published: 01 September 2008
Russ. Geol. Geophys. (2008) 49 (9): 655–666.
...) 18 7 2007 18 7 2007 © 2008, IGM, Siberian Branch of the RAS 2008 IGM, Siberian Branch of the RAS Pyrope-almandine garnets lower crust kimberlite shield Siberian Platform The study area is located in the eastern Siberian Platform, on the northwestern margin...
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Journal Article
Published: 01 July 2004
Russ. Geol. Geophys. (2004) 45 (7): 911–923.
...T.M. Parfenova; S.F. Bakhturov; Yu.Ya. Shabanov Applying modern analytical methods, we investigated organic matter from the Lower-Middle Cambrian rocks of the Kuonamka Formation in the eastern Siberian Platform. We divided the rocks into groups and subgroups according to the content of organic...
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Journal Article
Published: 01 July 2004
Russ. Geol. Geophys. (2004) 45 (7): 895–900.
...., there is good reason to consider them “genetically related”. The two above-mentioned families of naphthides are highlighted against the other genetic families of the eastern Siberian Platform in ratios of biomarker molecules and carbon isotope composition. In particular, quite an interesting picture emerges...
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Journal Article
Published: 01 November 1999
Russ. Geol. Geophys. (1999) 40 (11): 1672–1683.
... and biochemistry of initial living matter and physicogeographic conditions of its burial). It is shown that in the eastern Siberian Platform there were several time-variable centers of oil generation with different types of initial organic matter and physicogeographic conditions of sediment burial in major oil...
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Journal Article
Published: 01 August 1985
South African Journal of Geology (1985) 88 (2): 395–401.
Series: AAPG Studies in Geology
Published: 01 January 2013
DOI: 10.1306/13371591St643560
EISBN: 9781629812649
... potential of Russia’s vast heavy-oil and bitumen reserves is beginning to undergo systematic assessment, particularly in the eastern Siberian platform. Siberia’s natural bitumen fields have historically been disregarded and continue to be underrepresented in production markets mostly because of the climatic...
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Journal Article
Published: 01 October 2012
Russ. Geol. Geophys. (2012) 53 (10): 997–1011.
...–Elogui interfluve, in the eastern West Siberian Plate (eastern Khanty-Mansi Autonomous District). At a depth of 1790 m, they stripped a rhyolite extrusion, which graded into A -type alkali granitoids with rare-metal and REE mineralization (thorite, thorogummite, pitchblende, REE-carbonates, chevkinite...
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Journal Article
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1672–1679.
...B.F. Shevchenko; M.V. Goroshko; A.N. Didenko; V.A. Gur’yanov; V.S. Starosel’tsev; A.S. Sal’nikov Abstract The tectonic structure of the junction of the eastern Central Asian Fold Belt and the Siberian Platform, along with the deep structure of the Earth’s crust and lithosphere in this region, has...
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Journal Article
Published: 01 February 1996
Russ. Geol. Geophys. (1996) 37 (2): 14–22.
... reflection seismic horizons are given in Table 1 ; thus, there is a network of through reflection horizons KB, BP 2 , K 1 kn, K 1 kn, K 2 m, K 2 and K 3 . Table 1 Scheme of Correlation of Vendian-Cambrian Deposits of the Eastern Part of the Siberian Platform Eastern salt-forming region   Anab...
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Image
Middle Paleozoic structural stage of the eastern Siberian Platform. 1 — sedimentary basins with up to 1.5 km thick marine deposits; 2 — rifts composed of up to 6 km thick red-colored terrigenous evaporitic deposits; 3 — areas lacking Middle Paleozoic deposits; 4 — sites of small uplifts conjugate with rifts; 5 — uplifts conjugate with rifts (1 — Govorov, 2 — Dzhardzhan, 3 — Yakutian, 4 — Suntar); 6 — rifts (1 — Ygyatta, 2 — Kempendyai, 3 — Kyutyungde), 7 — kimberlites; 8 — faults and strike-slip faults; 9 — Muna-Markha interfluve (Parfenov and Kuz’min, 2001).
Published: 01 September 2008
Fig. 2. Middle Paleozoic structural stage of the eastern Siberian Platform. 1 — sedimentary basins with up to 1.5 km thick marine deposits; 2 — rifts composed of up to 6 km thick red-colored terrigenous evaporitic deposits; 3 — areas lacking Middle Paleozoic deposits; 4 — sites of small
Image
Tectonic scheme of the eastern Siberian Platform. 1, 2 – boundaries of: 1 – paleorift system, 2 – Vilyui-Markha zone; 3 – kimberlite fields: 1 – Malaya Botuobiya, 2 – Nakyn, 3 – Alakit, 4 – Daldyn, 5 – Muna.
Published: 01 December 1998
Fig. 1. Tectonic scheme of the eastern Siberian Platform. 1 , 2 – boundaries of: 1 – paleorift system, 2 – Vilyui-Markha zone; 3 – kimberlite fields: 1 – Malaya Botuobiya, 2 – Nakyn, 3 – Alakit, 4 – Daldyn, 5 – Muna.
Image
Wind-worn gold particles from platform areas (×300): a — eastern Siberian Platform; b — Russian Platform (materials by S.V. Yablokova, 1995); c — African Platform [14].
Published: 01 May 2005
Fig. 2. Wind-worn gold particles from platform areas (×300): a — eastern Siberian Platform; b — Russian Platform (materials by S.V. Yablokova, 1995); c — African Platform [ 14 ].
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1985
AAPG Bulletin (1985) 69 (2): 295.
... of the eastern Siberian platform and the south Siberian foldbelt. In Soviet terms, the age of the collection falls in a disputed interval called latest Early Cambrian (Tojonian) by some authors, and earliest Middle Cambrian (Amgan) by others. In North American terras, Macannaia is known only from early Middle...
Journal Article
Published: 01 August 2012
Russ. Geol. Geophys. (2012) 53 (8): 776–786.
..., the following trilobites were found: Triplagnostus gibbus , Tomagnostus sibiricus , Pseudanomocarina sp., Eodiscus oelandicus , Paradoxides sacheri , and Ptychagnostus aff. atavus . They are widespread in the vast territory of the eastern Siberian Platform, within the Kuonamka Formation. Also, Korobovia...
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Journal Article
Published: 01 July 2024
Russ. Geol. Geophys. (2024) 65 (7): 814–830.
...O.P. Polyansky; V.A. Simonov; O.V. Koroleva; A.V. Prokopiev; A.V. Babichev; A.V. Kotlyarov; A.N. Semenov Abstract —We report study results of basic intrusive bodies in the middle Paleozoic Vilyui paleorift (eastern Siberian Platform). Geochemical data for basic sills penetrated by boreholes...
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Journal Article
Published: 01 November 2020
Russ. Geol. Geophys. (2020) 61 (11): 1244–1259.
..., experiments, and analytical studies of the mineralogy of native gold. The objects of study were gold placers of the eastern Siberian Platform, Tuva, and Mongolia, gold-bearing conglomerates of the Timan Ridge, anthropogenic gold placers of the Yenisei Ridge, kaolinite and laterite weathering crusts of Salair...
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Journal Article
Journal: Geology
Published: 01 May 2017
Geology (2017) 45 (5): 459–462.
... chemostratigraphy and biostratigraphy for a terminal Ediacaran to Cambrian succession on the eastern Siberian Platform, Russia, which shows the presence of a succession of diverse fossil assemblages before the start of the basal Cambrian negative carbon isotope excursion (BACE). Soft-bodied Ediacaran biota...
FIGURES
Journal Article
Journal: Geology
Published: 01 January 2017
Geology (2017) 45 (1): 27–30.
... integrated to demonstrate cause and effect. Here we combine the record of macrofossils with early marine carbonate cement distribution within a relative depth framework for terminal Ediacaran to Cambrian successions on the eastern Siberian Platform, Russia, to interrogate the evolution of seawater chemistry...
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Journal Article
Published: 01 August 2011
Russ. Geol. Geophys. (2011) 52 (8): 773–780.
... conditions and the degree of maturity of OM containing lanostane and its derivates are considered. Lanostanes are proposed to use as biomarkers of the petroleum-generating rocks of the Sinyaya Formation for elucidating the source of naphthides in the eastern Siberian Platform. * Corresponding author. E...
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Image
Structures of the main biomarker molecules identified in oils and natural bitumens of the eastern Siberian Platform (the arrow indicates the most probable fragmentation from electron impact). I – 12- and 13-methyl alkanes (the most typical biomarkers for most of the oldest oils in the Siberian Platform); II – cheilanthanes; III – demethylated cheilanthanes (identified in the Permian bitumens of the Olenek uplift); IV – pregnane; V – steranes; VI – diasteranes; VII – hopanes; VIII – 25-norhopanes (identified in the Permian bitumens of the OIenek uplift); IX – 17α(H)-diahopane (typical biomarkers for oils of the Vilyui syneclise); X – gammacerane.
Published: 01 November 1999
Fig. 1. Structures of the main biomarker molecules identified in oils and natural bitumens of the eastern Siberian Platform (the arrow indicates the most probable fragmentation from electron impact). I – 12- and 13-methyl alkanes (the most typical biomarkers for most of the oldest oils