摘要
江西武夷山西坡中生代火山—斑岩形成于晚侏罗世—早白垩世 ,可分为南、北 2个火山—斑岩区、6个火山—斑岩带。指出了成矿火山—斑岩定性差别标志和控岩控矿构造 。
The volcanic porphyry of mesozoic era at Jiangxi Wuyi mountain west slope formed in late jurassic period early cretaceous period,it can divided into south and north volcanic porphyry region,six volcanic porphyry belt.The qualitative distinguish sign and structrue that control rock & ore of volcanic porphyry is point out,and its’ environment and cause of formation are approached.
出处
《江西冶金》
2000年第2期27-32,共6页
Jiangxi Metallurgy
关键词
中生代
火山-斑岩
成矿作用
江西武夷山西坡
mesozoic era
volcanic porphyry
mineralization
Jiangxi Wuyi mountain west slope
