NEW DATA ON THE STRUCTURE AND RADIOMETRIC AGE OF ROCKS OF THE LAPLAND GRANULITE BELT ON THE KANDALAKSHA COAST OF THE WHITE SEA

dc.contributor.author	Sukhanov M.K.
dc.contributor.author	Levitskiy V.I.
dc.contributor.author	Terekhov Y.N.
dc.date.accessioned	2020-04-16T07:05:02Z
dc.date.available	2020-04-16T07:05:02Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=31011499
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1987, 296, 5, 113-116
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16827
dc.description.abstract	Since the thermoisochron method requires only a small quantity of material (one or a few zircon crystals), the authors able for the first time to date sedimentary rocks and anorthosite that contain only very small quantities of zircon. For this purpose, zircons were extracted from all rock types of the granulite belt except garnet amphibolite, where they were not detected. Also dated were anorthosite and silicic granulite from the area around Lake Yavr in the northern part of this belt, as well as granite-gneiss from the White Sea block near Lake Khannus' yarvi. Study results are discussed.
dc.title	NEW DATA ON THE STRUCTURE AND RADIOMETRIC AGE OF ROCKS OF THE LAPLAND GRANULITE BELT ON THE KANDALAKSHA COAST OF THE WHITE SEA
dc.type	Статья

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