摘要
萨瓦亚尔顿金矿床成矿物质具有多源性。资料显示,主成矿元素金一部分来自矿区容矿地层,另一部分来自下伏地层,矿质S和C主要来自深部,特别是下伏火山岩;Pb来自于造山带。成矿溶液主要来自以大气降水为补给的地下(卤)水。
In the Shawayaerdun gold deposit of southwestern Tianshan, mineralizing material come from multiple source. According to study metallogenetic material, Au came from producing formation and underlying stratum, S-C from the depth underlaing volcanic zone and Pb from the orogenic zone. Mineralizing solution origined from underground hydrothermal brine water. They compensating from the precipitate water, meaning can not exclude the metamorphic water and magmatic water participation.
出处
《新疆地质》
CAS
CSCD
2001年第4期271-275,共5页
Xinjiang Geology
关键词
南天山西段
萨瓦亚尔顿金矿床
成矿物质
成矿元素
成矿溶液来源
the southwestern Tianshan
gold deposit of Shawayaerdun
mineralizing element
mineralizing solution
mineralizing material source
