THE AGE OF VOLCANIC SEQUENCE IN THE MIDDLE PALEOZOIC DEPOSITS OF SOUTHERN MONGOLIA

dc.contributor.author	Aristov V.A.
dc.contributor.author	Nyamsuren G.
dc.date.accessioned	2020-12-31T03:44:31Z
dc.date.available	2020-12-31T03:44:31Z
dc.date.issued	1998
dc.identifier	https://elibrary.ru/item.asp?id=13299472
dc.identifier.citation	Stratigraphy and Geological Correlation, 1998, , 1, 92-96
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21856
dc.description.abstract	Recent finds of conodonts indicate that the volcanogenic sequence in the Gobi Altai-Suhe Bator Zone of southern Mongolia (the Gobi Altai Formation in the Dzhinsetu Ulul Range area and the Minzhin Formation in the Mandai Obo area), earlier regarded as barren of fossils, was formed in the interval between the Givetian of the Middle Devonian and the early Fammennian of the Late Devonian. The ratio of effusive and volcaniclastic rocks in the studied sections suggests that centers of volcanism moved from east to west during the indicated period.
dc.subject	Paleozoic	en
dc.title	THE AGE OF VOLCANIC SEQUENCE IN THE MIDDLE PALEOZOIC DEPOSITS OF SOUTHERN MONGOLIA
dc.type	Статья
dc.subject.age	Paleozoic	en
dc.subject.age	Палеозой	ru

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