Fluid inclusion study of gold-bearing quartz-sulphide veins and cassiterite from the Czarnow As deposit ore (SW Poland)

被引：0
|
作者：
Mikulski, S. Z. [1 ]
Kozlowski, A.
Speczik, S. [1 ]
机构：
[1] Polish Geol Inst, PL-00975 Warsaw, Poland
来源：
DIGGING DEEPER, VOLS 1 AND 2: DIGGING DEEPER | 2007年
关键词：
gold; cassiterite; fluid inclusion; Czarnow; Rudawy Janowickie Mountains; Western Sudetes; SW Poland; Bohemian massif; European Variscides;
D O I：
暂无
中图分类号：
P5 [地质学];
学科分类号：
0709 ; 081803 ;
摘要：
Primary fluid inclusions in three generations of auriferous quartz from the Czarnow As deposit were examined. Two first generations of investigated quartz contain refractory and non-refractory gold. The major auriferous period of mineralization occurred in temperatures from 400 to 200 degrees C, while lowest temperature quartz-late carbonate mineralization is devoid of gold. In the ore assemblage cassiterite was an early mineral, which formed at 440-384 and 340-315 degrees C, under pressure 1.2-1.1 kbar from liquid solutions of the total salinity 24-16 wt. % of NaCl equivalent.
引用
收藏
页码：805 / 808
页数：4
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