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Data · dataset · 2001

Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals

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Rare-metal alkali (quartz-feldspathic) metasomatites are considered in terms of their geologic position, structure, and composition.

Description

Their petrochemical and geochemical characteristics are given. In the Polar Urals, the metasomatites occur as lenticular and tube-like bodies in the fault zones of the Cambrian basement within the Kharbey block.

Three types of the metasomatites, dated at ~300 Ma, have been recognised: quartz-bifeldspathic (kvalmites), quarzt-albitic, and albitites. They belong to the formation of quartz-feldspathic metasomatites of the fault zones.

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Geology 74%
Provenance · 1 source records, 7 field assertions
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DataCite10.1594/pangaea.10728112 d agoJSON v1
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