RARE EARTH ELEMENTS IN THE ROCKS OF THE GERANSKIY ANORTHOSITE PLUTON

dc.contributor.authorSukhanov M.K.
dc.contributor.authorBogdanova N.G.
dc.contributor.authorLyapunov S.M.
dc.contributor.authorYermolayev B.V.
dc.date.accessioned2020-11-02T00:30:44Z
dc.date.available2020-11-02T00:30:44Z
dc.date.issued1990
dc.description.abstractAnalysis of the distribution of REE in the rocks of the Geranskiy pluton suggests the following: 1) in comparison with anorthosites of autonomous type in other regions [9, 11], the rocks of the Geranskiy pluton differ in their higher REE contents and in this respect are closest to anorthosites of the anorthosite-granite association [10], 2) it confirms the existence of a latent internal layering of the series of anorthosites of the main phase, which crystallized from high-alumina melts and at first glance appear to be uniform.
dc.identifierhttps://elibrary.ru/item.asp?id=31148407
dc.identifier.citationTransactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 1, 184-187
dc.identifier.issn0891-5571
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/18354
dc.titleRARE EARTH ELEMENTS IN THE ROCKS OF THE GERANSKIY ANORTHOSITE PLUTON
dc.typeСтатья

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