Литология и особенности формирования кембрийских отложений в юго-восточной части Западно-Сибирской геосинеклизы А. Е. Ковешников, В. А. Конторович, С. Н. Макаренко [и др.]
Material type:
ArticleOther title: Lithology and features of formation the lower Cambrian deposits in south-east part of the West Siberian geosyneclise [Parallel title]Subject(s): кембрийские отложения | Западно-Сибирская геосинеклиза | литология кембрийских отложенийGenre/Form: статьи в сборниках Online resources: Click here to access online
In:
Эволюция жизни на Земле : материалы V Международного симпозиума, 12-16 ноября 2018 г С. 67-69Abstract: In the South-Eastern part of West-Siberian geosineklise in recent years established distribution Cambrian sediments is
greater than previously thought, the territory. Study of the conditions of accumulation Cambrian formations becomes relevant in
connection with a possible association with him deposits of oil and gas. Objective of the study is based on the study of faunal
remains a reliable and establishing the presence of Cambrian deposits on the territory of Nurolsky structural-facial regionstudying
the peculiarities of the lithological composition of sediments and the conditions of their formation with the purpose of
revealing of features of their propagation. The formation of the carbonate platforms, which are represented by the dolomites,
whose accumulation at the end of the early Cambrian period, perhaps, closer to the end of the Cambrian, it stopped.
Библиогр.: 6 назв.
In the South-Eastern part of West-Siberian geosineklise in recent years established distribution Cambrian sediments is
greater than previously thought, the territory. Study of the conditions of accumulation Cambrian formations becomes relevant in
connection with a possible association with him deposits of oil and gas. Objective of the study is based on the study of faunal
remains a reliable and establishing the presence of Cambrian deposits on the territory of Nurolsky structural-facial regionstudying
the peculiarities of the lithological composition of sediments and the conditions of their formation with the purpose of
revealing of features of their propagation. The formation of the carbonate platforms, which are represented by the dolomites,
whose accumulation at the end of the early Cambrian period, perhaps, closer to the end of the Cambrian, it stopped.
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