敦煌地块变质岩系时代新认识

    NEW SPECULATION OF THE AGE OF THE METAMORPHIC ROCK SERIES OF THE DUNHANG MASSIF

    • 摘要: 敦煌地块的中深变质岩系敦煌群,经1/5万区调获得Sm-Nd等时线年龄值2935Ma、2946Ma、3487Ma,归属于太古界。北山南带的中深一浅变质岩系,经1/5万区调及1/20万区调修测,在中深变质岩系中获得Sm-Nd等时线年龄值2949Ma、2956Ma、3237Ma及2203Ma、2059Ma,分别划归敦煌群和厘定为早元古代。在浅变质岩系中获得Sm-Nd等时线年龄值1622Ma、1624Ma及Baicalia等叠层石,归属于中上元古界。

       

      Abstract: During 1:50000 regional surveys.the Dunhuang Group of the intermediate-and high- grademetamorphic rock series in the Dunhuang massif was determined to have Sm-Nd isochron age val-ues of 2935Ma , 2946Ma and 3487Ma,belonging to the Archean, Samples from the intermediate-and high-grade metamorpnic rock series in the south zone of the Beishan Mounains gave Sm-Ndisochron age values of 2949Ma,2956Ma,3237Ma ,2203Ma and 2059Ma,which are respectively as-signed to the Dunhuang Group and determined to be of Proterozoic age. Stromatolites such asBaicaliia were collected from the low-grade rock series and ages of 1622 Ma were obtained,so theseries is assigned to the middle Upper Proterozic.

       

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