Unique paragenesis of cerium and yttrium allanites in tourmalinite of the Severny massif (Chukotka)


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Abstract

A description of hydrothermal allanite-(Y) and its unique association with allanite-(Ce) from tourmaline metasomatic rock of the Severny granite massif in Chukotka is presented in the article. Examination of the composition of metasomatic rims in allanite-(Y) allowed us to estimate the limit of isomorphic replacement in allanite of Y and heavy lanthanides by LREE, reaching 25%.

About the authors

V. I. Alekseev

Saint-Petersburg Mining University

Author for correspondence.
Email: wia59@mail.ru
Russian Federation, St. Petersburg

Yu. B. Marin

Saint-Petersburg Mining University

Email: wia59@mail.ru
Russian Federation, St. Petersburg

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