THE OPTIMAL NUMBER OF CARBONIFEROUS SERIES AND STAGES

dc.contributor.author	Menning M.
dc.contributor.author	Belka Z.
dc.contributor.author	Chuvashov B.
dc.contributor.author	Engel B.A.
dc.contributor.author	Jones P.J.
dc.contributor.author	Kullmann J.
dc.contributor.author	Utting J.
dc.contributor.author	Watney L.
dc.contributor.author	Weyer D.
dc.date.accessioned	2021-02-14T10:44:32Z
dc.date.available	2021-02-14T10:44:32Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=13366080
dc.identifier.citation	Newsletters on Stratigraphy, 2001, 38, 2-3, 201-207
dc.identifier.issn	0078-0421
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24982
dc.description.abstract	The number of global Carboniferous series and stages should be consistent with those of the neighbouring Devonian and Permian systems. Therefore, two series and seven to nine stages are preferred instead of two subsystems, seven to nine series, and 21 to 35 stages.
dc.subject	Carboniferous
dc.title	THE OPTIMAL NUMBER OF CARBONIFEROUS SERIES AND STAGES
dc.type	Статья
dc.subject.age	Палеозой::Каменноугольная	ru
dc.subject.age	Paleozoic::Carboniferous	en

Files in this item

Files	Size	Format	View
There are no files associated with this item.