摘要
千鹅冲钼矿床是新近发现的一特大型钼矿床。产于桐柏—商城断裂带的北侧,矿体受断裂和隐伏花岗岩体控制。通过对矿床成矿地质条件、矿化及蚀变特征分析,认为该矿床为斑岩型钼矿,燕山期花岗斑岩为其成矿母岩。
Qian＇ e＇ chong Mo deposit is a newly discovered oversize Mo deposit, which occurs on tt^e nortn slae of Tongbo-Shangcheng fracture belt and is controlled by fracture and concealed granite mass. The analysis on geologic condition of mineralization and characteristics of mineralization and alteration suggests that the deposit is a porphyry Mo deposit and granite porphyry in Yanshan phase is its metallizing mother rock.
出处
《矿产与地质》
2013年第2期126-131,共6页
Mineral Resources and Geology
关键词
钼矿床
地质特征
找矿标志
光山千鹅冲
河南
Mo deposit, geological characteristic, clues for prospecting, Qian ＇ e ＇ chong in Guangshan, Henan
