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Zircon SHRIMP U-Pb Dating of the Tourmalinites from Boron-bearing Series of Borate Deposits in Eastern Liaoning and its Geological Implications

查看全文 作  者:LIU [1,2]Jingdang;XIAO [3]Rongge;ZHANG [1,2]Yanfei;FAN [1]Minghui;WANG [1]Shengzhi;JIA [1]Yuguo;WANG [1]Gang;LIU [4]Zhixue 高影响力作者 机构地区:[1]Liaoning Geological Survey for Chemical Industry,Jinzhou 121000,Liaoning,China;[2]Liaoning Technical University,Fuxin 123000,Liaoning,China;[3]School of the Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China;[4]Liaoning Mining Exchange Center,Shenyang 110013,Liaoning,China高影响力机构 出  处:《Acta Geologica Sinica(English Edition)》索引2012年第86卷第1期,共13页高影响力期刊 基  金:supported by the National Natural Science Foundation of China grant(40073013) 摘  要:This paper focused on the zircon sensitive high resolution ion micro-probeU-Pb geochronology of the tourmalinites from boron-bearing series of borate deposits in Eastern Liaoning.The zircons commonly have core-rim structures,most cores show oscillatory zoning in cathodoluminescence and plane polarized light images,suggesting a magmatic detrital origin.Ages of the magmatic detrital zircons from the hyalotourmalite samples(N13) and(N14) are 2175±5Ma and 2171±9Ma,respectively.Moreover,metamorphic zircon from the sample(N13) shows an age of 1906±4Ma.Zircon core and rim from the hyalotourmalite sample(N02) record ages of 2171±6Ma and 1889±62Ma,which are explained as indicating the formation and metamorphic ages.Combined with the geological and geochemical studies,it can be concluded that the tourmalinites are formed during sedimentary exhalative mineralizations in the mid-Paleoproterozoic(~2170Ma) and underwent the metamorphism in the late-Paleoproterozoic(~1900Ma).The tourmalinites are the products of submarine acid volcanism in the extension rifting phase of the Liaoji Paleoproterozoic Rift,the rock-forming materials of which are derived from the mantle sources with recycling crustal contamination.The emergence of tourmalinites not only indicates the mid-Paleoproterozoic tectonic-magmatic processes,but also provides impetus,heat and material sources for the mineralization of borate deposits in Eastern Liaoning. 关 键 词:SHRIMP锆石U-PB年龄 地质意义 硼酸 存款 轴承 辽东 U-PB年代学 古元古代
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