Lithologic-petrographic features and conditions of regional cyclite J15 rock formation, revealed by parametrical well 1st Western-Tomsk area

Bibliographic Details
Parent link:Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007
Vol. 310, № 1.— 2007.— [P. 20-24]
Other Authors: Osipova E. N. Elizaveta Nikolaevna, Ezhova A. V. Aleksandra Viktorovna, Nedolivko N. M. Nataliya Mikhailovna, Perevertaylo (Perevertailo) T. G. Tatyana Gennadievna, Polumogina Е. D.
Summary:Заглавие с титульного листа
Электронная версия печатной публикации
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.
Published: 2007
Series:Earth science
Subjects:
Online Access:http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v310eng/i1/04.pdf
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=180470

MARC

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200 1 |a Lithologic-petrographic features and conditions of regional cyclite J15 rock formation, revealed by parametrical well 1st Western-Tomsk area  |f Е. N. Osipova [et al.] 
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320 |a [Bibliography: p. 24 (5 titles)] 
330 |a 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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461 1 |0 (RuTPU)RU\TPU\book\169973  |t Bulletin of the Tomsk Polytechnic University  |f Tomsk Polytechnic University (TPU)  |d 2006-2007 
463 1 |0 (RuTPU)RU\TPU\book\195457  |t Vol. 310, № 1  |v [P. 20-24]  |d 2007  |p 201 p. 
610 1 |a lithologic-petrographic features 
610 1 |a conditions 
610 1 |a formation 
610 1 |a regional cyclite 
610 1 |a parametrical wells 
610 1 |a lithologic-petrographic researches 
610 1 |a transgressive cycles 
610 1 |a lithological structure 
610 1 |a zonal cyclitis 
610 1 |a chlorites 
610 1 |a glauconites 
610 1 |a organic fossils 
610 1 |a faunae 
610 1 |a stratification 
610 1 |a washout 
610 1 |a redeposition 
610 1 |a sediments 
610 1 |a shallow marine basin 
610 1 |a hydrodynamic modes 
610 1 |a труды учёных ТПУ 
610 1 |a электронный ресурс 
675 |a 552.5:551.862.1  |v 3 
701 1 |a Osipova  |b E. N.  |c Geologist  |c Senior Lecturer at Tomsk Polytechnic University, Candidate of Geological and Mineralogical Sciences  |f 1960-  |g Elizaveta Nikolaevna  |3 (RuTPU)RU\TPU\pers\33265  |9 17010 
701 1 |a Ezhova  |b A. V.  |c geologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences  |f 1939-  |g Aleksandra Viktorovna  |3 (RuTPU)RU\TPU\pers\33997 
701 1 |a Nedolivko  |b N. M.  |c geologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences  |f 1955-  |g Nataliya Mikhailovna  |3 (RuTPU)RU\TPU\pers\34027  |9 17594 
701 1 |a Perevertaylo (Perevertailo)  |b T. G.  |c geologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences  |f 1969-  |g Tatyana Gennadievna  |3 (RuTPU)RU\TPU\pers\34026  |9 17593 
701 1 |a Polumogina  |b Е. D. 
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