NATIVE METALS IN LAMPROITES OF THE CENTRAL ALDAN

dc.contributor.author	Kononova V.A.
dc.contributor.author	Makhotkin I.L.
dc.contributor.author	Dmitriyeva M.T.
dc.contributor.author	Yeremeyev N.V.
dc.contributor.author	Aleshin V.G.
dc.contributor.author	Vashchenko A.N.
dc.date.accessioned	2020-04-15T06:24:13Z
dc.date.available	2020-04-15T06:24:13Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30976486
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 303, 6, 167-171
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16727
dc.description.abstract	Rocks of the lamproite series, like kimberlites, are products of very deep processes and extreme enrichment of the upper mantle. They are now being studied far more widely because of diamond finds in lamproites of Australia. Although no native metal finds in lamproites are mentioned in Soviet or foreign publications, there are reports of native metal finds in lamproitic rocks of Central Asia. This publication is the first description of native metals and their alloys in rocks of the lamproite series. Lamproitic igneous activity in the Soviet Union was most complete and diverse at the south margin of the Siberian craton, where the Aldan lamproite province of Mesozoic age is distinguished.
dc.subject	Mesozoic	en
dc.title	NATIVE METALS IN LAMPROITES OF THE CENTRAL ALDAN
dc.type	Статья
dc.subject.age	Mesozoic	en
dc.subject.age	Мезозой	ru

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