Types of gold mineralization at Suzdal sediment-hosted gold deposit in East Kazakhstan

被引：0
|
作者：
Kovalev, K. R. [1 ]
Naumov, E. A. [1 ]
Kalinin, Yu. A. [1 ]
Tretjakova, I. G. [1 ]
Borisenko, A. S. [1 ]
Kolesnikova, M. [1 ]
机构：
[1] RAS, Inst Geol & Mineral, Novosibirsk 630090, Russia
来源：
DIGGING DEEPER, VOLS 1 AND 2: DIGGING DEEPER | 2007年
关键词：
disseminated gold; carbonaceous terrigeneous-carbonate rocks; poligenetic type ores; mineralogy of gold mineralization;
D O I：
暂无
中图分类号：
P5 [地质学];
学科分类号：
0709 ; 081803 ;
摘要：
The Suzdal gold-sulphide deposit, characterized by fine gold hosted in Carboniferous-aged carbonaceous-terrigeneous-carbonate lithologies, is located in the Kalba gold-bearing belt in the eastern Kazakhstan. Three types of mineralized rocks are distinguished: 1) sedimentary and melange calcareous breccias, 2) silicified tectonic breccias of sulphidized carbonaceous-terrigeneous rocks, and 3) sulphidized sandstones and carbonaceous siltstones. The first two types contain native gold. The third one contains invisible gold, which occurs preferentially in stellar-aggregated arsenopyrite and is chemically bonded.
引用
收藏
页码：569 / 572
页数：4
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