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《Geochimica》 1993-04
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GEOCHRONOLOGY OF THE SHUANGSHANZI AND ZHUZHANGZI GROUPS,QINGLONG,EASTERN HEBEI

Wang Qichao (Shijiazhuang Comprehensive Geological Party,Shijiazhuang,050081)Zhang Shaoqing Ren Shuxiang (Hebei Regional Geological Survey Team,Langfang,102800)  
In isotopic dating this paper emphasizes the role of fluids in isotopic rehomo-genization during metamorphism.Sedimentary metamorphic rocks are abundant inconnate water and the dating of clastic zircon yields,in most cases,the age ofmetamorphism and deformation.In some cases the Sm-Nd isochron ages of igneousrocks are also relatively low.All this may be related to the incorporation of mixedwater during low-temperature diaphthoresis.It is concluded,based on the availableU-Pb ages,Rb-Sr isochron ages and Sm-Nd ages(including the whole-rock isochronand mortal ages)in conjunction of the geochronology data of global greenstones,thatthe Shuangshaazi and Zhuzhangzi groups should be Late Neoarchaean in age,rangingfrom 2450 to 2650 Ma.
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