THE EVOLUTION OF PRE-MESOZOIC OPHIOLITES IN NORTHERN EURASIA: A COMPARATIVE REVIEW

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dc.contributor.author Dobretsov N.L.
dc.contributor.author Zonenshain L.P.
dc.date.accessioned 2020-10-02T08:41:53Z
dc.date.available 2020-10-02T08:41:53Z
dc.date.issued 1989
dc.identifier https://elibrary.ru/item.asp?id=30942618
dc.identifier.citation CHEMICAL GEOLOGY, 1989, 77, 3-4, 323-330
dc.identifier.issn 0009-2541
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/17601
dc.description.abstract In this paper we will compare the Riphean (Late Proterozoic) ophiolites of the North Baikalian region and Polar Urals of the Bohemian and Saxonian granulite massifs, the Paleozoic ophiolites of West and East Sayan, Urals, Stara Planina and Polish Sudetes, etc. In these examples the similarity of the main stages of the tectonic evolution of the Paleoasiatic and Iapetus oceans is shown. It is clear that the majority of them had a multistage evolution in oceanic, back-arc or ensimatic arc condition. Further, the general scheme of this evolution is shown.
dc.subject Mesozoic en
dc.title THE EVOLUTION OF PRE-MESOZOIC OPHIOLITES IN NORTHERN EURASIA: A COMPARATIVE REVIEW
dc.type Статья
dc.subject.age Mesozoic en
dc.subject.age Мезозой ru


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