ASSOCIATIONS OF CENOZOIC BASALTIC ROCKS IN THE SEA OF JAPAN

dc.contributor.author	S'yedin V.T.
dc.date.accessioned	2020-04-15T06:24:14Z
dc.date.available	2020-04-15T06:24:14Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=30976770
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1987, 296, 5, 124-128
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16738
dc.description.abstract	This article describes Cenozoic basaltic rocks in the Sea of Japan. Analysis of a large body of data leads to a division of them into natural associations of volcanic rocks and specific geochemical types. Their classification is based on the chemical properties of these rocks and their minerals, taking into account the mode of evolution of the parental basalt magma, and on their relationship to different morphostructures in the Sea of Japan. There are four associations of Cenozoic basaltic rocks here: 1) continental tholeiites; 2) island-arc volcanics; 3) basaltic rocks of marginal seas, i.e., tholeiites and related differentiates; 4) alkalic basaltic volcanics of the type characteristic of continental rifts.
dc.subject	Cenozoic	en
dc.title	ASSOCIATIONS OF CENOZOIC BASALTIC ROCKS IN THE SEA OF JAPAN
dc.type	Статья
dc.subject.age	Cenozoic	en
dc.subject.age	Кайнозой	ru

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