摘要
薄刀岭银矿为大别地区发现的重要中型银矿床之一,与矿区内薄刀岭岩体密切相关。地球化学数据显示薄刀岭二长花岗岩为过铝质高钾钙碱性I型花岗岩,具富碱明显、相对富钾的特征。岩体LA-ICP-MS锆石U-Pb测年为(144.0±1.1)Ma,属早白垩世,为该时期大别地区整体挤压局部伸展环境的产物。
Bodaoling Silver Mine is one of the important medium-sized silver deposits found in Dabie area,which is closely related to the Bodaoling rock mass.Geochemical data prove that the monzonitic is peraluminous high-potassium calcium-alkali type I granite,which is obviously alkali rich and potassium-rich.The LA-ICP-MS zircon U-Pb age of the granite is(144.0±1.1)Ma,which was formed in the Early Cretaceous due to overall compression and local extensional environment in Dabie area.
作者
王海生
WANG Haisheng(No.3 Institute of Geological&Mineral Resources Survey of Henan Geological Bureau,Zhengzhou450008,China)
出处
《四川有色金属》
2020年第3期38-42,共5页
Sichuan Nonferrous Metals
关键词
薄刀岭银矿
锆石U-PB定年
地球化学
Bodaoling silver mine
Zircon U-Pb age
geochemical characteristics