摘要
江西浒坑钨矿为与燕山早期花岗岩有关的岩浆热液矿床,以充填石英脉型钨矿为主,偶有云英岩型钨矿化。矿床在后期先后遭受了韧性和脆性变形,形成了条带状含矿石英脉。
The Hukeng tungsten deposit of Jiangxi Province formed in the early Yanshan Geological Period is genetically related to magmatism.The mineralization of tungsten is mainly quartz vein type,as well as some greisenization type occasionally.The tungsten deposit had been undergone ductile and brittle deformation and formed banded ore bearing quartz vein.
出处
《江西有色金属》
2009年第4期3-7,共5页
Jiangxi Nonferrous Metals
关键词
石英脉型
韧性变形
脆性变形
条带状
浒坑钨矿
quartz vein type
ductile and brittle deformation
banded structure
Hukeng tungsten deposit
