摘要
云雾岭铜矿化产于燕山期复式花岗岩岩体中 ,初步认为属斑岩型 ,具较大成矿规模和找矿远景 。
The porphyritic copper mineralization in Yunwuning of Xinjiang was discovered for the first time in June of 1996by searching boulders. The mineralization occurs in biotite- plagiogranite porphyrites of Yanshanian composite granites,which is the western extension of Jinshajiang - Honghe Yanshanian por- phyritic copper( molybdenum) metallogenic belt,with a large metallogenic scale and a good prospect. In cou- ple with the recent work in Datong and Bulunkou of Kunlun mountains,the study assumes thata Yanshanian porphyritic copper( molybdenum) metallogenic belt exists along Yunwuning of Kunlun mountains in the southern Xinjiang.So a further work is needed.
出处
《新疆地质》
CAS
CSCD
1998年第2期185-187,共3页
Xinjiang Geology
关键词
新疆
云雾岭
铜矿化
发现
意义
Xinjiang Yunwuning copper mineralization discovery significance
