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Andreicheva, L N (2007): Composition of sedimentary rocks from the Shapkina River valley, Bolshezemelskaya Tundra [dataset publication series]. Institute of Geology, Komi Scientific Cener, Ural Division, Russian Academy of Sciences, PANGAEA, https://doi.org/10.1594/PANGAEA.784066, Supplement to: Andreicheva, LN (2007): Pleistocene sediments in the Shapkina River valley (Bol'shaya Zemlya Tundra). Translated from Litologiya i Poleznye Iskopaemye, 2007, 1, 93-110, Lithology and Mineral Resources, 42(1), 84-100, https://doi.org/10.1134/S0024490207010099

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Published: 2007 (exact date unknown) • DOI registered: 2012-07-11

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Abstract:
A facies-genetic and stratigraphic subdivision of the Quaternary sequence in the Shapkina River valley has been accomplished. The riverbank shows outcrops of three glacial complexes with different mineralogical-petrographic compositions and structural characteristics, which can be correlated and stratificated. Datings of intermoraine horizons (alluvial, marine, lacustrine, and lacustrine-boggy sediments) have been based on palynological and paleomicrotheriological data. The Middle Neopleistocene section can be divided into two till horizons corresponding to two autonomous glaciations (Pechora and Vychegda). They are separated by a member of subaqueous Rodionov sediments. The Pechora till formed in the course of glacier motions from the northeast. Glacial horizons are mainly composed of the Vychegda till transported from the Northwest terrigenous provenance. Lithology of the Upper Neopleistocene Polyarnyi till testifies to its formation in the upper course of the river from material transported from the Northeast terrigenous-mineralogical provenance in the upper course of the river and from the Fennoscandian glaciation center in the lower course of the river. The paper presents the first lithological investigation and substantiation of genesis of various facies of Neopleistocene intermoraine marine sediments (sediments of the beach and fore-beach zones and shallow-water shelf).
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 67.098133 * Median Longitude: 53.883523 * South-bound Latitude: 66.800000 * West-bound Longitude: 53.210000 * North-bound Latitude: 67.510000 * East-bound Longitude: 54.710000
Event(s):
ShRV-1 * Latitude: 67.510000 * Longitude: 54.630000 * Location: Bolshezemelskaya Tundra
ShRV-2 * Latitude: 67.460000 * Longitude: 54.710000 * Location: Bolshezemelskaya Tundra
ShRV-3 * Latitude: 67.460000 * Longitude: 54.500000 * Location: Bolshezemelskaya Tundra
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4 datasets

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Datasets listed in this publication series

  1. Andreicheva, LN (2007): (Table 2) Petrographic composition of coarse clastic material from tills of the Shapkina River valley. https://doi.org/10.1594/PANGAEA.784062
  2. Andreicheva, LN (2007): (Table 3) Composition of heavy minerals in sediments of the Rodionov Horizon from the Shapkina River valley. https://doi.org/10.1594/PANGAEA.784063
  3. Andreicheva, LN (2007): (Table 4) Composition of heavy minerals in fluvioglacial sediments from the Shapkina River valley. https://doi.org/10.1594/PANGAEA.784064
  4. Andreicheva, LN (2007): (Table 5) Composition of heavy minerals in marine sandy loams from the Shapkina River valley. https://doi.org/10.1594/PANGAEA.784065