The distribution of rare-earth elements in orebodies of the dzhimidon base-metal deposit and in the host rocks in North Ossetia, Russia

The sources of material that make up veins at hydrothermal deposits were estimated by distribution of REE in ores and host rocks. Paleozoic granites (major ore-hosting rocks at most deposits) and Precambrian schists (ore-hosting rocks typical only of the Dzhimidon deposit), which are the predominant...

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Published inMoscow University geology bulletin Vol. 66; no. 4; pp. 269 - 273
Main Authors Borisov, M. V., Volkova, M. M., Bychkov, D. A., Bychkova, Ya. V.
Format Journal Article
LanguageEnglish
Published Heidelberg Allerton Press, Inc 01.08.2011
Springer Nature B.V
Subjects
Earth and Environmental Science
Earth Sciences
Geology
Metals
Paleozoic
Precambrian
Rare earth elements
Rocks
Trace elements
North Ossetia Russia
Russia
rare-earth elements
and base-metal vein deposits
sources of ore material
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Summary:The sources of material that make up veins at hydrothermal deposits were estimated by distribution of REE in ores and host rocks. Paleozoic granites (major ore-hosting rocks at most deposits) and Precambrian schists (ore-hosting rocks typical only of the Dzhimidon deposit), which are the predominant rocks of the Sadon district, played an important role in the formation of base-metal ores.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0145-8752
1934-8436
DOI:10.3103/S014587521104003X