THE AGE OF CHOKUSU BEDS IN THE KYZYL-DZHAR-CHOKUSU SECTION (THE SILURIAN OF NORTHWESTERN MONGOLIA)

dc.contributor.author	Bondarenko O.B.
dc.contributor.author	Minzhin C.
dc.date.accessioned	2021-01-28T11:13:03Z
dc.date.available	2021-01-28T11:13:03Z
dc.date.issued	2000
dc.identifier	https://elibrary.ru/item.asp?id=13346433
dc.identifier.citation	Stratigraphy and Geological Correlation, 2000, 8, 3, 243-255
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/23887
dc.description.abstract	The rock succession and age of the Chokusu Beds in the Mt. Kyzyl-Dzhar-Chokusu section is considered to be either the Ludlovian-Pridolian or Wenlockian-early Ludlovian. The discrepancy resulted from a complicated geological structure and contradictory interpretations of rock ages on the basis of different groups of invertebrates (tabulates, heliolitids, rugoses, bryozoans, brachiopods). We reckon the beds to be of the Wenlockian age. It is not inconceivable that the upper Llandoverian and lower Ludlovian deposits are also present in the section.
dc.subject	Silurian	en
dc.title	THE AGE OF CHOKUSU BEDS IN THE KYZYL-DZHAR-CHOKUSU SECTION (THE SILURIAN OF NORTHWESTERN MONGOLIA)
dc.type	Статья
dc.subject.age	Paleozoic::Silurian	en
dc.subject.age	Палеозой::Силурийская	ru

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