ЛЮМИНЕСЦЕНЦИЯ ПЛАГИОКЛАЗОВ ИЗ ГОРНЫХ ПОРОД НЕКОТОРЫХ ДРЕВНИХ СТРУКТУРНЫХ ЗОН ЕВРОПЕЙСКОГО КОНТИНЕНТА

dc.contributor.author	Морошкин В.В.
dc.date.accessioned	2024-04-06T00:47:25Z
dc.date.available	2024-04-06T00:47:25Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=9438958
dc.identifier.citation	Записки Российского минералогического общества, 2006, 135, 4, 65-80
dc.identifier.issn	0869-6055
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/43381
dc.description.abstract	Luminescence was studied for plagioclascs from various types of sialic rocks occurring within large consolidated structures of Precambrian basement - crystalline shields of East-European platform, and the so called «median massifs» (Zwischengcbirgc) in the folded areas of Central and West Europe. Some general regularities of the luminescence variations (degree of participating for different luminogens) reflect peculiarities of tecto-no-magmatic and gcochcmical evolution as of separate regional structures, so of the common geologic-tectonic history of continental crust for the whole European continent.
dc.title	ЛЮМИНЕСЦЕНЦИЯ ПЛАГИОКЛАЗОВ ИЗ ГОРНЫХ ПОРОД НЕКОТОРЫХ ДРЕВНИХ СТРУКТУРНЫХ ЗОН ЕВРОПЕЙСКОГО КОНТИНЕНТА
dc.type	Статья
dc.subject.udc	549:535.37
dc.subject.age	Палеозой::Кембрийская
dc.subject.age	Докембрий

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