The U–Pb System in Schorlomite from Calcite–Amphobole–Pyroxene Pegmatite of the Afrikanda Complex (Kola Peninsula)


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The geochronological U–Pb study of shorlomite from igneous rocks of the alkali–ultramafic Afrikanda massif (Kola Peninsula) was performed. The results demonstrate the reliability of calcium garnet as a mineral for the U–Pb geochronology of a wide range of igneous rocks, i.e., carbonatite, syenite, foidolite, foidite, melilitolite, melilitite, lamprophyres, micaceous kimberlites, etc., and associated rare earth and trace elements (REE, Nb, Zr) mineralization.

作者简介

E. Salnikova

Institute of Precambrian Geology and Geochronology

编辑信件的主要联系方式.
Email: katesalnikova@yandex.ru
俄罗斯联邦, St. Petersburg, 199034

M. Stifeeva

Institute of Precambrian Geology and Geochronology

Email: katesalnikova@yandex.ru
俄罗斯联邦, St. Petersburg, 199034

A. Chakhmouradian

University of Manitoba

Email: katesalnikova@yandex.ru
加拿大, Winnipeg

V. Glebovitsky

Institute of Precambrian Geology and Geochronology

Email: katesalnikova@yandex.ru
俄罗斯联邦, St. Petersburg, 199034

E. Reguir

University of Manitoba

Email: katesalnikova@yandex.ru
加拿大, Winnipeg

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