ЗАКОНОМЕРНЫЕ СРАСТАНИЯ МИНЕРАЛОВ В ПЕГМАТИТАХ ИЛЬМЕНСКИХ ГОР

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dc.contributor.author Попов В.А.
dc.contributor.author Попова В.И.
dc.contributor.author Поляков В.О.
dc.date.accessioned 2024-03-30T02:42:18Z
dc.date.available 2024-03-30T02:42:18Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=9301074
dc.identifier.citation Записки Российского минералогического общества, 2006, 135, 5, 48-59
dc.identifier.issn 0869-6055
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/43236
dc.description.abstract The paper summarized results of investigations of the oriented intergrowths of minerals within pegmatites of the Ilmeny mountains. There are two-feldspars, two-micas, biotite-amphibolc, biotite-pyroxene and pyroxe-ne-amphibole intergrowths revealed in syenite (feldspar and nepheline-feldspar) pegmatites. Orientation of the cxsolution products was studied in "sunstonc" (avcnturine feldspar) and "moonstone" feldspars, nephelines and cancrinites. Corundum-biotitc-feldspar and two-micas intergrowths and exsolutions are characterized in star-co-rundums from corundum-feldspar veins. Syntaxic intergrowths of various amphiboles and chlorites were remarked in pegmatoid ultramafites. The regular quartz-feldspar (graphic) and two-feldspars intergrowths are typical for granite pegmatites; there were also detected two-micas, columbite-samarskite and columbite-ilmenorutile, zircon-xenotime, cassiterite-ilmenorutile and cassiterite-ixiolitc, cassiterite-tantalite, tantalite-stibiotantalite, fer-gusonitc-columbite, pyrochlore-fcrgusonite and beryl-cordierite intergrowths. New laws of intergrowth have been revealed for many pairs of minerals.
dc.title ЗАКОНОМЕРНЫЕ СРАСТАНИЯ МИНЕРАЛОВ В ПЕГМАТИТАХ ИЛЬМЕНСКИХ ГОР
dc.type Статья
dc.subject.udc 549:548:552.322


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