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    Volume 30 Issue 4
    Jul.  2005
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    ZHANG Hong, LIU Xiao-ming, ZHANG Ye-qing, YUAN Hong-lin, HU Zhao-chu, 2005. Zircon U-Pb Ages and Significance of Bottom and Top Beds ofZhangjiakou Formation in Liaoning and Hebei Provinces. Earth Science, 30(4): 387-401.
    Citation: ZHANG Hong, LIU Xiao-ming, ZHANG Ye-qing, YUAN Hong-lin, HU Zhao-chu, 2005. Zircon U-Pb Ages and Significance of Bottom and Top Beds ofZhangjiakou Formation in Liaoning and Hebei Provinces. Earth Science, 30(4): 387-401.

    Zircon U-Pb Ages and Significance of Bottom and Top Beds ofZhangjiakou Formation in Liaoning and Hebei Provinces

    • Received Date: 2005-04-12
    • Publish Date: 2005-07-25
    • In Lingyuan region,Liaoning Province,the Zhangjiakou Formation and the Lower Mesozoic strata are in an ENE orientation,while the Yixian Formation is NNE orientated,the two formations are angular unconformity.According to the new U-Pb isotopic age analysis of zircon by LA-ICP-MS,the bottom bed of the Zhangjiakou Formation in Lingyuan is about 132 Ma,and the top bed is about 129.5-130 Ma.In Luanping region,Hebei Province,the bottom bed of the Zhangjiakou Formation is about 136 Ma,and the top bed is about 135 Ma.The Zhangjiakou Formation in the Lingyuan and Luanping regions is comparable,which reflects that the volcanic rock of the Zhangjiakou Formation from Luanping to Lingyuan becomes younger in time.The top bed of the Zhangjiakou Formation in Lingyuan has about a 5-6 Ma interval with the bottom bed of Yixian Formation,which proves that the angular unconformity of Zhangjiakou Formation and Yixian Formation is credible; suggesting that the 5-6 Ma interval period is the main period of the transition of tectonic framework in the Mesozoic in Hebei and Liaoning provinces.In the interval period,the magnetic action went up to high tide in the Mesozoic in the northeast of China.Moreover,after the interval period,the Rehe fauna developed into the erupted period,which also reflects that the interval period is an important biological interface in Hebei and Liaoning provinces.According to the isotopic age,the Dabeigou Formation in Luanping region corresponds to the upper bed of the Zhangjiakou Formation,not to the bottom bed of the Yixian Formation.

       

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