KFU. Card publication. Zorina S.O. Mesozoic Platform Megasequences in the Eastern Part of the Russian Plate. In: R.Rocha, J.Pais, J.C.Kullberg, S.Finney (Eds.). STRATI 2013. First International Congress on Stratigraphy. At the Cutting Edge of Stratigraphy. Springer Geology 2014, pp. 821-824. DOI: 10.1007/978-3-319-04364-7

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ZORINA S.O. MESOZOIC PLATFORM MEGASEQUENCES IN THE EASTERN PART OF THE RUSSIAN PLATE. IN: R.ROCHA, J.PAIS, J.C.KULLBERG, S.FINNEY (EDS.). STRATI 2013. FIRST INTERNATIONAL CONGRESS ON STRATIGRAPHY. AT THE CUTTING EDGE OF STRATIGRAPHY. SPRINGER GEOLOGY 2014, PP. 821-824. DOI: 10.1007/978-3-319-04364-7_154

Form of presentation

International monographs

Year of publication

2014

Authors, employees of KFU

Zorina Svetlana Olegovna, author

Bibliographic description in the original language

Zorina S.O. Mesozoic Platform Megasequences in the Eastern Part of the Russian Plate. In: R.Rocha, J.Pais, J.C.Kullberg, S.Finney (Eds.). STRATI 2013. First International Congress on Stratigraphy. At the Cutting Edge of Stratigraphy. Springer Geology. Part XIV. 2014, pp. 821-824. DOI: 10.1007/978-3-319-04364-7_154

Annotation

On the basis of investigations of the sequences and chronostratigraphy of the Middle Jurassic-Lower Cretaceous deposits in the eastern part of the Russian Plate, five megasequences are identified: the upper Bajocian?Callovian, Oxfordian?Berriasian, Valanginian, upper Hauterivian?Aptian, and Albian megasequences. These were formed under stable tectonic-eustatic conditions (without long breaks in sedimentation). The megasequences are characterized by peculiar sediment compositions: mineral assemblages are specific to individual horizons, units, or the entire megasequence, and they include a specific complex of solid mineral resources.

Keywords

Sequence stratigraphy, Chronostratigraphy, Megasequences, Solid mineral resources

URL

http://www.springer.com/earth+sciences+and+geography/geology/book/978-3-319-04363-0

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=80863&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Zorina Svetlana Olegovna	ru_RU
dc.date.accessioned	2014-01-01T00:00:00Z	ru_RU
dc.date.available	2014-01-01T00:00:00Z	ru_RU
dc.date.issued	2014	ru_RU
dc.identifier.citation	Zorina S.O. Mesozoic Platform Megasequences in the Eastern Part of the Russian Plate. In: R.Rocha, J.Pais, J.C.Kullberg, S.Finney (Eds.). STRATI 2013. First International Congress on Stratigraphy. At the Cutting Edge of Stratigraphy. Springer Geology. Part XIV. 2014, pp. 821-824. DOI: 10.1007/978-3-319-04364-7_154	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=80863&p_lang=2	ru_RU
dc.description.abstract	On the basis of investigations of the sequences and chronostratigraphy of the Middle Jurassic-Lower Cretaceous deposits in the eastern part of the Russian Plate, five megasequences are identified: the upper Bajocian?Callovian, Oxfordian?Berriasian, Valanginian, upper Hauterivian?Aptian, and Albian megasequences. These were formed under stable tectonic-eustatic conditions (without long breaks in sedimentation). The megasequences are characterized by peculiar sediment compositions: mineral assemblages are specific to individual horizons, units, or the entire megasequence, and they include a specific complex of solid mineral resources.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Sequence stratigraphy	ru_RU
dc.subject	Chronostratigraphy	ru_RU
dc.subject	Megasequences	ru_RU
dc.subject	Solid mineral resources	ru_RU
dc.title	Zorina S.O. Mesozoic Platform Megasequences in the Eastern Part of the Russian Plate. In: R.Rocha, J.Pais, J.C.Kullberg, S.Finney (Eds.). STRATI 2013. First International Congress on Stratigraphy. At the Cutting Edge of Stratigraphy. Springer Geology 2014, pp. 821-824. DOI: 10.1007/978-3-319-04364-7_154	ru_RU
dc.type	International monographs	ru_RU