Lithologic-petrographic features and conditions of regional cyclite J15 rock formation, revealed by parametrical well 1st Western-Tomsk area; Bulletin of the Tomsk Polytechnic University; Vol. 310, № 1

Lithologic-petrographic features and conditions of regional cyclite J15 rock formation, revealed by parametrical well 1st Western-Tomsk area; Bulletin of the Tomsk Polytechnic University; Vol. 310, № 1

Opis bibliograficzny
Parent link:Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007
Vol. 310, № 1.— 2007.— [P. 20-24]
Kolejni autorzy: Osipova E. N. Elizaveta Nikolaevna, Ezhova A. V. Aleksandra Viktorovna, Nedolivko N. M. Nataliya Mikhailovna, Perevertaylo (Perevertailo) T. G. Tatyana Gennadievna, Polumogina Е. D.
Streszczenie: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.
Język:angielski
Wydane: 2007
Seria:Earth science
Hasła przedmiotowe:
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
Dostęp online:http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v310eng/i1/04.pdf
Format: Elektroniczne Rozdział
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=180470
Opis
Opis fizyczny:1 файл (2.5 Мб)
Streszczenie: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.

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