HIGH-PRECISION U-PB ZIRCON GEOCHRONOLOGY AND THE STRATIGRAPHIC RECORD

dc.contributor.author	Bowring S.A.
dc.contributor.author	Schmitz M.D.
dc.date.accessioned	2021-12-02T03:58:08Z
dc.date.available	2021-12-02T03:58:08Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=14468614
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2003, 53, , 53
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/32649
dc.description.abstract	The rock stratigraphic record exists as a rich, albeit complex and incomplete repository of Earth history, tracing the processes of biological evolution, climate change, oceanic and atmo-spheric chemistry, sea-level fluctuations, mountain-building and erosion, and basin subsidence. Without a detailed and precise temporal framework, however, the richness of the record, including global stratigraphic correlations, evaluation of cyclicity and rates of regional and global change, major sedimentary depositional hiatuses, and biological extinctions cannot be fully exploited.
dc.title	HIGH-PRECISION U-PB ZIRCON GEOCHRONOLOGY AND THE STRATIGRAPHIC RECORD
dc.type	Статья

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