Discovery and metallogenesis of the Antuoling Mo deposit and its implications
1 IntroductionThe Antuoling Mo deposit is the most achievement of Tianjin North China Geological Exploration General Institute, China. The ore district is located at the North Segment of the Taihang intraplate orogen, between the Dahenanian and Laiyuanian batholiths. The cropped out strata in the district are mainly the Archean metamorphic rocks of the Fuping group and the Mid-Late Proterozoic carbonate rocks. There are a minor granitic intrusion and many dikes, which characterized by wide spectrum of chemical compositions (Fig. 1). As early as at the middle of 1980s, some favourable clues for copper exploration were discovered in this area. However, the works are not successive till recent years. Recently, the mining engineers have discovered molybdenum ore bodies in the surrounding metamorphic rocks of the minor intrusion. The workable reserves of molybdenum metal are 0.15 Mt.
Luo Zhaohua Fan Binghong Lu Shuwen Cheng Suhua Zhand Qing Liang Tao
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Tianjin North China Geological Exploration General Institute, Tianjin 300181, China
国际会议
Xian International Ni-Cu(Pt) Deposit Symposium 2009(2009 西安·Ni-Cu(Pt)岩浆矿床国际学术研讨会)
西安
英文
214-217
2009-09-01（万方平台首次上网日期，不代表论文的发表时间）