摘要
过去一直认为西华山黑钨矿石英脉是高中温热液充填而成。研究发现 ,在黑钨矿石英脉的绿柱石中存在与流体 (气液 )包裹体共生的流体 -熔体包裹体和熔融包裹体 ,这表明形成黑钨矿石英脉的成矿流体是一种岩浆 -热液过渡性流体。
It used to be considered that the wolframite quartz veins in Xihuashan orefield had be crystallized from hyperthermal or mesothermal solution. Reported here are fluid melt inclusions and silicate inclusions within beryl of the wolframite quartz veins, coexisting with gas liquid inclusions, which suggests that the metallogenetic fluids be a magmatic hydrothermal solution.
出处
《华南地质与矿产》
CAS
2001年第2期21-27,共7页
Geology and Mineral Resources of South China
关键词
黑钨矿石英脉
熔融包裹体
成矿流体
岩浆-热液流体
江西
绿柱石
钨矿床
wolframite quartz veins melt inclusion metallogenetic fluids magma hydrothermal fluid Xihuashan orefield Jiangxi
