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Lithology, geochemistry, and aspects of separation of the Kogalym Member within the Lower Vasyugan Subhorizon (Upper Bathonian-Lowermost Oxfordian) of West Siberia

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dc.contributor.author Yan P.
dc.contributor.author Vakulenko L.
dc.contributor.author Kostyreva E.
dc.contributor.author Aukhatov Y.
dc.contributor.author Burleva O.
dc.contributor.author Nikolenko O.
dc.date.accessioned 2018-09-19T20:58:19Z
dc.date.available 2018-09-19T20:58:19Z
dc.date.issued 2017
dc.identifier.issn 1068-7971
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/143473
dc.description.abstract © 2017It is proposed to separate a regionally persistent member of fine-dispersed mudstones as the individual Kogalym Member within the Lower Vasyugan Subhorizon (Uppermost Bathonian-Lowermost Oxfordian). We present data on the lithologic composition, geophysical characteristics, and geochemical properties of the organic matter and depositional environments of the member. The Tyumenskaya SG-6 well is proposed as a type section of the Kogalym Member, where a biostratigraphic approach has yielded the Middle-Upper Callovian volume of the member. We also discuss the aspects of specification and detalization of the Callovain-Oxfordian part of the Callovian and Upper Jurassic regional scheme of West Siberia.
dc.relation.ispartofseries Russian Geology and Geophysics
dc.subject Callovian
dc.subject geochemical composition of organic matter
dc.subject lithology
dc.subject Oxfordian
dc.subject regional stratigraphy
dc.subject Vasyugan Horizon
dc.subject West Siberia
dc.title Lithology, geochemistry, and aspects of separation of the Kogalym Member within the Lower Vasyugan Subhorizon (Upper Bathonian-Lowermost Oxfordian) of West Siberia
dc.type Article
dc.relation.ispartofseries-issue 3-4
dc.relation.ispartofseries-volume 58
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 393
dc.source.id SCOPUS10687971-2017-58-34-SID85018501637


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  • Публикации сотрудников КФУ Scopus [24551]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

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