Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals, supplement to: Udoratina, Oxana V (2001): Alkali-Metasomatites from the Polar Urals. Polarforschung, 69, 143-148

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

Metasomatites have been dated at about 300 Million years.

Identifier
DOI https://doi.org/10.1594/PANGAEA.107281
PID https://hdl.handle.net/10013/epic.29837.d001
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.107281
Provenance
Creator Udoratina, Oxana V
Publisher PANGAEA - Data Publisher for Earth & Environmental Science
Publication Year 2001
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 997 data points
Discipline Earth System Research
Spatial Coverage (65.900 LON, 67.300 LAT); Ural