TIME-CORRELATION OF LATE PERMIAN STRATIGRAPHIC SEQUENCES

dc.contributor.author	Shang Q.
dc.contributor.author	Cao C.
dc.contributor.author	Jin Y.
dc.date.accessioned	2022-07-16T04:12:11Z
dc.date.available	2022-07-16T04:12:11Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=32195072
dc.identifier.citation	Acta Geologica Sinica (English Edition), 2004, 78, 4, 448-457
dc.identifier.issn	1000-9515
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38160
dc.description.abstract	The Upper Permian recorded the greatest mass extinction and the most dramatic environmental changes in geologic history. Understanding the process of these events has long been handicapped by the uncertainty of their synchronity of Late Permian sequences in major depositional regions. With the Lopingian Series as the global standard for the Upper Permian and a set of bio-, magneto- and sequence stratigraphic tie points, a global correlation of Lopingian rocks at stage-level is tentatively suggested.
dc.subject	Permian
dc.title	TIME-CORRELATION OF LATE PERMIAN STRATIGRAPHIC SEQUENCES
dc.type	Статья
dc.subject.age	Paleozoic::Permian
dc.subject.age	Палеозой::Пермская	ru

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