吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1552-1569.doi: 10.13278/j.cnki.jjuese.20200120
• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇 下一篇
智云宝1, 孙海瑞2,3, 李风华1
Zhi Yunbao1, Sun Hairui2,3, Li Fenghua1
摘要: 笏山金矿床为陡崖断裂带南段内最大的金矿床,为了揭示其矿床成因,在矿床地质研究的基础上开展了矿体围岩元素地球化学和流体包裹体研究。研究结果表明:笏山金矿床沿NE向断裂发育大规模的热液蚀变带,地表出露的断裂带形成一个庞大的面形蚀变带,矿化较弱,分带不明显,钻孔显示金矿体两侧依次发育黄铁绢英岩、绢英岩化花岗岩蚀变带和二长花岗岩,金矿体主要产于陡崖断裂带下盘黄铁绢英岩蚀变带内。质量平衡计算表明:绢英岩化过程中,主量元素SiO2、Al2O3、FeO、MnO、Na2O、K2O、P2O5和部分稀土元素从二长花岗岩中迁出,而MgO、CaO、Fe2O3,成矿元素Au、Ag,亲硫元素Cu、Pb及亲铁元素V、Cr、Co、Ni迁入二长花岗岩;黄铁绢英岩化过程中,主量元素FeO、Fe2O3、MnO、MgO、CaO,成矿元素Au、Ag,亲硫元素Cu及亲铁元素V、Cr、Co、Ni迁入,SiO2、Al2O3、Na2O、K2O和P2O5迁出。岩相学观察、显微测温以及单个包裹体成分激光拉曼分析提示其流体包裹体类型主要为气液两相包裹体和含CO2三相包裹体,具有低盐度(w(NaCl)为5.33%~13.29%)和中温(260~300℃)CO2-NaCl-H2O体系,在成矿过程中,含矿流体经历了流体不混溶作用。结合矿床地质特征及实验结果分析,确定该矿床为受陡崖断裂带控制的中温蚀变岩型金矿床。
中图分类号:
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