TRENDS IN DEVELOPMENT OF LATE DEVONIAN REEFS

dc.contributor.author	Kuznetsov V.G.
dc.date.accessioned	2021-06-11T04:57:56Z
dc.date.available	2021-06-11T04:57:56Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=13410638
dc.identifier.citation	Stratigraphy and Geological Correlation, 2002, 10, 5, 441-459
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/29032
dc.description.abstract	The Late Devonian was a period of degraded reef formation that was very intense in the Middle Paleozoic. Principal reef-building organisms, such as stromatoporoids, rugoses, and tabulates of the Frasnian Stage, were replaced by Famennian cyanobacteria and algae at that time. This resulted in development of Famennian frameless buildups instead of Frasnian framework reefs since the late Frasnian through the early Famennian. The difference in tectonic settings of reef development in continental and oceanic stratisphere segments is established. In oceanic segments, the frameless reefs were likely formed earlier than in continental settings.
dc.subject	Devonian
dc.title	TRENDS IN DEVELOPMENT OF LATE DEVONIAN REEFS
dc.type	Статья
dc.subject.age	Paleozoic::Devonian
dc.subject.age	Палеозой::Девонская	ru

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