Paleogeographic and litho-facies formation conditions of MidUpper Jurassic sediments in S-E Western Siberia (Tomsk Oblast); IOP Conference Series: Earth and Environmental Science; Vol. 43 : Problems of Geology and Subsurface Development

Manylion Llyfryddiaeth
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012001, 5 p.]
Prif Awdur: Shaminova M. I. Marina Ivanovna
Awdur Corfforaethol: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра общей геологии и землеустройства (ОГЗ)
Awduron Eraill: Rychkova I. V. Irina Vladimirovna, Sterzhanova Ju.
Crynodeb:Title screen
This paper describes the criteria to identify Tumen (lower Bathonian) and Naunak (upper Bathonian-Callovian- Oxfordian) suites within S-E Western Siberia (Tomsk Oblast). The specific paleogeographic and litho-facies formation conditions of sediments and numerous vegetable remains and ichnofossils indicated the fact that this territory was the location of sedimentogenesis transition during Tumen and Naunak suite formation. Based on integrated survey oil-gas potential litho-facies groups were defined in Mid-Upper Jurassic sediments within S-E Western Siberia.
Iaith:Saesneg
Cyhoeddwyd: 2016
Cyfres:Mineralogy, Geochemistry and Petrography
Pynciau:
Mynediad Ar-lein:http://dx.doi.org/10.1088/1755-1315/43/1/012001
http://earchive.tpu.ru/handle/11683/35119
Fformat: Electronig Pennod Llyfr
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650794

MARC

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200 1 |a Paleogeographic and litho-facies formation conditions of MidUpper Jurassic sediments in S-E Western Siberia (Tomsk Oblast)  |f M. I. Shaminova, I. V. Rychkova, Ju. Sterzhanova 
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330 |a This paper describes the criteria to identify Tumen (lower Bathonian) and Naunak (upper Bathonian-Callovian- Oxfordian) suites within S-E Western Siberia (Tomsk Oblast). The specific paleogeographic and litho-facies formation conditions of sediments and numerous vegetable remains and ichnofossils indicated the fact that this territory was the location of sedimentogenesis transition during Tumen and Naunak suite formation. Based on integrated survey oil-gas potential litho-facies groups were defined in Mid-Upper Jurassic sediments within S-E Western Siberia. 
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