THE PERMO-TRIASSIC "PALEOTETHYS" IN MAINLAND SOUTHEAST-ASIA AND ADJACENT PARTS OF CHINA

dc.contributor.author	Helmcke D.
dc.date.accessioned	2020-02-22T08:34:35Z
dc.date.available	2020-02-22T08:34:35Z
dc.date.issued	1985
dc.identifier	https://elibrary.ru/item.asp?id=31163604
dc.identifier.citation	INTERNATIONAL JOURNAL OF EARTH SCIENCES, 1985, 74, 2, 215-228
dc.identifier.issn	1437-3254
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/15998
dc.description.abstract	Aspects of the geodynamic evolution of mainland Southeast Asia and China are discussed in consideration of the Permo-Triassic »Paleotethys« problem. It is shown that all sutures in Thailand, Vietnam and Yunnan already closed during the Paleozoic era and that the entire region must be regarded as part of the northern continents. The Permo-Triassic »Paleotethys« must be expected south of Tibet and in Burma.
dc.subject	Triassic	en
dc.title	THE PERMO-TRIASSIC "PALEOTETHYS" IN MAINLAND SOUTHEAST-ASIA AND ADJACENT PARTS OF CHINA
dc.type	Статья
dc.subject.age	Mesozoic::Triassic	en
dc.subject.age	Мезозой::Триасовая	ru

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