REE distribution in zircon from reference rocks of the Arctic region: Evidence from study by the LA-ICP-MS method


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The results of the LA-ICP-MS analysis of the concentrations of REEs, U, Th, and Hf in zircon from Paleo- and Neoarchean reference rocks of the Kola region (garnet–amphibole gneiss, basic and acid granulites, and granite pegmatite) are reported. A new methodology of the study of accessory zircons has been validated and modified. The accuracy of the results is confirmed by analysis of standard zircons Temora 1 and 91 500 and by comparison with the data obtained in other laboratories.

作者简介

A. Nikolaev

Tananaev Institute of Chemistry and Technology of Rare Elements and Mineral Raw Materials, Kola Science Center

Email: drogo_sv@chemy.kolasc.net.ru
俄罗斯联邦, Apatity, Murmansk oblast

S. Drogobuzhskaya

Tananaev Institute of Chemistry and Technology of Rare Elements and Mineral Raw Materials, Kola Science Center

编辑信件的主要联系方式.
Email: drogo_sv@chemy.kolasc.net.ru
俄罗斯联邦, Apatity, Murmansk oblast

T. Bayanova

Geological Institute, Kola Science Center

Email: drogo_sv@chemy.kolasc.net.ru
俄罗斯联邦, Apatity, Murmansk oblast

T. Kaulina

Geological Institute, Kola Science Center

Email: drogo_sv@chemy.kolasc.net.ru
俄罗斯联邦, Apatity, Murmansk oblast

L. Lyalina

Geological Institute, Kola Science Center

Email: drogo_sv@chemy.kolasc.net.ru
俄罗斯联邦, Apatity, Murmansk oblast

A. Novikov

Tananaev Institute of Chemistry and Technology of Rare Elements and Mineral Raw Materials, Kola Science Center

Email: drogo_sv@chemy.kolasc.net.ru
俄罗斯联邦, Apatity, Murmansk oblast

E. Steshenko

Geological Institute, Kola Science Center

Email: drogo_sv@chemy.kolasc.net.ru
俄罗斯联邦, Apatity, Murmansk oblast

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