The Distribution of Rare-Earth Elements in Orebodies of the Dzhimidon Base-Metal Deposit and in the Host Rocks in North Ossetia, Russia

被引：0

作者：

Borisov, M. V. ^{[1
]}

Volkova, M. M. ^{[1
]}

Bychkov, D. A. ^{[1
]}

Bychkova, Ya. V. ^{[2
]}

机构：

[1] Moscow MV Lomonosov State Univ, Fac Geol, Geochem Dept, Moscow 119899, Russia

[2] Russian Acad Sci, Vernadsky Inst Geochem & Analyt Chem, Moscow 119991, Russia

来源：

MOSCOW UNIVERSITY GEOLOGY BULLETIN | 2011年 / 66卷 / 04期

基金：

俄罗斯基础研究基金会;

关键词：

rare-earth elements; sources of ore material; and base-metal vein deposits;

D O I：

10.3103/S014587521104003X

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

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 Pre-cambrian 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.

引用

页码：269 / 273

页数：5

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