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Mayanian

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Journal Article
Published: 01 January 2008
Russ. Geol. Geophys. (2008) 49 (1): 1–22.
...V.V. Khomentovsky; K.E. Nagovitsin; A.A. Postnikov Abstract The Mayanian (1100–850 Ma) is an all-Siberian stratigraphic subdivision of the Neoproterozoic distinguished on the basis of generalized geological and paleontological data for the Maya Group in the southeast of the Siberian craton...
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Journal Article
Published: 01 July 2006
Russ. Geol. Geophys. (2006) 47 (7): 865–880.
... of these structures can be, in turn, divided into several structure-facies zones. As in the south, three main stages of development have been established in the Neoproterozoic of the above structural elements, which correspond to the Mayanian, Baikalian, and Vendian. The most considerable modifications are made...
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Schematic general paleogeologic profile of <span class="search-highlight">Mayanian</span> in Uchur-Yudoma SFA (ge...
Published: 01 January 2008
Fig. 2. Schematic general paleogeologic profile of Mayanian in Uchur-Yudoma SFA (generalization of profiles after ( Khomentovsky, 2005 )). 1 — dolomites; 2 — limestones; 3 — clayey-carbonate rocks; 4 — silt- and mudstones; 5 — sandstones; 6 — gravelstones and conglomerates; 7
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Schematic Neoproterozoic paleostructure of Northern Taimyr.  1  — flysch (U...
Published: 01 July 2006
— Kolosov Formation, carbonates (Kerpylian(?)-Lakhandinian); 5 — Kan’yon Formation, siltstones, mudstones (Lakhandinian); 6 — Posadochnaya Formation, clastics (Lower Vendian(?)); 7 — terrigenous-carbonate deposits (Upper Vendian-Cambrian); 8 — Borzov series, volcanics (Mayanian); 9 — ophiolites
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Schematic location of structure-facies features of <span class="search-highlight">Mayanian</span>.  1, 2  — intra...
Published: 01 January 2008
Fig. 1. Schematic location of structure-facies features of Mayanian. 1, 2 — intracratonic depressions, 3, 4 — pericratonic troughs: 1, 3 — outlined according to outcrops and boreholes, 2, 4 — tentative contour beneath younger deposits; 5 — marginal oceanic blocks; 6 — microcontinents
Journal Article
Published: 01 May 2005
Russ. Geol. Geophys. (2005) 46 (5): 529–545.
... been established for all these structures, but the location and nature of boundaries between them as well as their age are still debatable. The information available casts doubt upon many universally accepted concepts. It is proven that the Maya Group giving rise to the Mayanian, the lower...
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Journal Article
Published: 01 September 2007
Russ. Geol. Geophys. (2007) 48 (9): 711–720.
... here the Mayanian. The fundamentally different nature of the events associated with the next, Baikalian stage of the development allows its tripartite subdivision in the region. Deposition of the Lower Baikalian (the Oslyanka Group) was preceded by the crustal extension at the junction between...
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Schematic reconstruction of the Upper Riphean paleostructure of the Yenisei...
Published: 01 September 2007
Fig. 1. Schematic reconstruction of the Upper Riphean paleostructure of the Yenisei Range and adjacent part of the Mid-Angara depression. 1–6 — structural features of the Mayanian in the Yenisei pericratonic trough: 1 — Predbol’shepatomskoe uplift composed chiefly of Early Precambrian
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Schematic paleogeologic profile of pre-Vendian deposits of Baikal-Lena SFA....
Published: 01 January 2008
Fig. 3. Schematic paleogeologic profile of pre-Vendian deposits of Baikal-Lena SFA. After: Khomentovskii and Postnikov (2001) with corrections. 1 — Early Precambrian; 2 — symbols of Late Precambrian formations. Lower and Middle Riphean: pp — Purpol’, md — Medvezh’ya, ok — Okun’. Mayanian
Journal Article
Published: 01 July 2006
Russ. Geol. Geophys. (2006) 47 (7): 913–916.
... were used to argument for his principal statements: “The age of the oceanic volcanosedimentary and volcanogenic deposits in the Chukchi-Borzov and Zhdanov structure-facies zones is essentially refined. It is proven (stressed by me — V.V.) that they correspond to the Mayanian alone” (p. 862). “Vast...
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Schematic paleogeologic profiles of deposits of Neoproterozoic of Yenisei-A...
Published: 01 January 2008
— Upper Kamo Subgroup (Formations): tk — Tokur, ir — Iremeken. Mayanian deposits: in Kamenka and Gorbilok SFZ, Formations: pg — Pogoryui, kr — Kartochki, al — Alad’ino, kg — Krasnogorsk, dj — Dzhura, šn —Shuntar, sk — Seryi Klyuch, dd — Dadykta; in Gorbilok SFZ: pt — Potoskui (pt 1 , pt 2 — Lower
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Schematic correlation between sections of the Riphean deposits (southern pr...
Published: 01 May 2005
and gravelstones; 9 — conglomerates and gravelstones; 10 — group boundaries; 11 — formation boundaries; 12 — washouts; 13 — angular discordances; 14 — crystalline basement; 15 — symbolized stratigraphic units: V — Vendian, Yudoma Group; bk — Baikalian, Ui Group; mn — Mayanian, Maya Group: lh
Journal Article
Published: 01 March 2014
Russ. Geol. Geophys. (2014) 55 (3): 361–368.
... Groups. The Kirgitei Subgroup with distinct age boundaries is distinguished in the upper Tungusik Group ( Khomentovsky, 2007 ). The Kerpylian and Lakhandinian Horizons are combined into the Mayanian, which is an all-Siberian stratigraphic subdivision ( Khomentovsky, 1996 ; Khomentovsky et al., 2008...
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Schematic paleogeological profiles of Neoproterozoic pre-Late Baikalian-Ven...
Published: 01 September 2007
Subgroup, formations: tk — Tokur, ir — Iremeken; Mayanian deposits: Bol’shoi Pit Group in Kamenka SFZ, formations: pg — Pogoryui, kr — Kartochka, al — Alad’in, kg — Krasnaya Gorka, dj — Dzhura, sk — Seryi Klyuch, dd — Dadykta; in Gorbilok SFZ: pt — Potoskui Formation, pt1 — Lower Potoskui Subformation, pt2
Journal Article
Published: 01 November 2010
Russ. Geol. Geophys. (2010) 51 (11): 1192–1198.
... (Russian Geology and Geophysics) 39 ( 10 ), 1365 – 1376 (1366–1377) . Khomentovsky , V.V. , Nagovitsin , K.E , Postnikov , A.A. , 2008 . Mayanian (1100–850 Ma)–Prebaikalian Upper Riphean of Siberia . Russian Geology and Geophysics (Geologiya i Geofizika) 49 ( 1 ), 1 – 22 (3...
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Journal Article
Published: 01 September 2011
Journal of Paleontology (2011) 85 (5): 987–1011.
... succession of the Siberian platform was early on subdivided into a series of Regional Stratigraphic units considered as the types for potentially global biostratigraphic subdivisions of the later Proterozoic Eon: the Uiaian, Aimchanian, Mayanian (Kerpylian and Lakhandinian), and Baikalian ( Khomentovsky et...
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