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河南光山县千鹅冲钼矿床围岩蚀变与成矿规律
引用本文:王海生. 河南光山县千鹅冲钼矿床围岩蚀变与成矿规律[J]. 四川地质学报, 2013, 0(3): 291-294
作者姓名:王海生
作者单位:河南省地矿局第三地质矿产调查院,河南 信阳,464000
摘    要:河南光山县千鹅冲矿床属于癍岩型钼矿床。矿床围岩蚀变硅化、钾长石化、黄铁矿化、绢云母化、绿帘及绿泥石化、高岭土化等多叠加出现,强弱不等。其中硅化、钾长石化、绢云母化、黄铁矿化发育较强且与矿化关系密切。研究表明:在岩浆期后的各成矿阶段,石英、钾长石、磁铁矿、辉钼矿、含矿流体等经过充填、沉淀,在岩体上部围岩中形成了多期矿化细脉叠加、范围集中、规模巨大的钼矿体。

关 键 词:围岩蚀变  钼矿床  斑岩  光山千鹅冲

Study of Wall Rock Alteration and Ore-formation of the Qianhechong Mo Deposit in Guangshan, Henan
WANG Hai-sheng. Study of Wall Rock Alteration and Ore-formation of the Qianhechong Mo Deposit in Guangshan, Henan[J]. Acta Geologica Sichuan, 2013, 0(3): 291-294
Authors:WANG Hai-sheng
Affiliation:WANG Hai-sheng (No.3 Geological Survey, Henan Bureau of Geology and Mineral Resources, Xinyang, Henan 464000)
Abstract:The Qianhechong Mo Deposit in Guangshan, Henan is a porphyry Mo one. The wall-rock alteration is characterized by silicification, potash feldspathization, pyritization, sericitization, epidotization, chloritization and kaolinization. The Mo mineralization was in close relationship with silicification, potash feldspathization, sericitization and pyritization.
Keywords:wall-rock alteration  Mo deposit  porphyry  Qianhechong,Guangshan
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