Lithologic-petrographic features and conditions of regional cyclite J15 rock formation, revealed by parametrical well 1st Western-Tomsk area [Electronic resource] / Е. N. Osipova [et al.]

Уровень набора: (RuTPU)RU\TPU\book\169973, Bulletin of the Tomsk Polytechnic University / Tomsk Polytechnic University (TPU) = 2006-2007Альтернативный автор-лицо: Osipova, E. N., Geologist, Assistant of the Department of Tomsk Polytechnic University, 1960-, Elizaveta Nikolaevna;Ezhova, A. V., geologist, Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences, 1939-, Aleksandra Viktorovna;Nedolivko, N. M., geologist, Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences, 1955-, Nataliya Mikhailovna;Perevertaylo (Perevertailo), T. G., geologist, Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences, 1969-, Tatyana Gennadievna;Polumogina, Е. D.Язык: английский ; оригинала, русский.Страна: Россия.Описание: 1 файл (2.5 Мб)Серия: Earth scienceРезюме или реферат: The implemented lithologic-petrographic researches have shown that formation of regional cyclitis U15 rocks, revealed by the parametrical well 1 of the Western-Tomsk area (Tomsk region), occurred during two alternating transgressive cycles, features of which are reflected in lithological structure of lower and upper zonal cyclitis. Inclusions of glauconite and chlorite, organic fossils, faunae, various stratification, washout and redeposition traces of underlaying sediments indicates the formation of the studied strata in shallow marine basin with an active hydrodynamic mode..Примечания о наличии в документе библиографии/указателя: [Bibliography: p. 24 (5 titles)].Тематика: lithologic-petrographic features | conditions | formation | regional cyclite | parametrical wells | lithologic-petrographic researches | transgressive cycles | lithological structure | zonal cyclitis | chlorites | glauconites | organic fossils | faunae | stratification | washout | redeposition | sediments | shallow marine basin | hydrodynamic modes | труды учёных ТПУ | электронный ресурс Ресурсы он-лайн:Щелкните здесь для доступа в онлайн
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[Bibliography: p. 24 (5 titles)]

The implemented lithologic-petrographic researches have shown that formation of regional cyclitis U15 rocks, revealed by the parametrical well 1 of the Western-Tomsk area (Tomsk region), occurred during two alternating transgressive cycles, features of which are reflected in lithological structure of lower and upper zonal cyclitis. Inclusions of glauconite and chlorite, organic fossils, faunae, various stratification, washout and redeposition traces of underlaying sediments indicates the formation of the studied strata in shallow marine basin with an active hydrodynamic mode.

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