Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (2): 471-482.doi: 10.13278/j.cnki.jjuese.201502111

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U-Pb Isotopic Age of the Volcanic Rocks of the Yixian Formation in Jianping Machang of Western Liaoning and Its Geological Significance

Chen Jingsheng1,2, Li Weiwei3, Liu Miao1,2, Xing Dehe2, Yang Jialin2   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Shenyang Institute of Geology and Mineral Resources/Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China;
    3. Liaoning Institute of Geology and Mineral Resources, Shenyang 110029, China
  • Received:2014-07-16 Published:2015-03-26

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Abstract:

Yixian Formation volcanic rocks widely exists in Jianping Machang in western Liaoning. Through the study of the measured sections,three volcanic eruption cycles(early,middle and late) have been recognized. A new LA-ICP-MS zircon U-Pb dating of the volcanic rocks in different cycle presents three ages for the three cycles: (the early age (127.7±1.8)-(124.3±1.8) Ma, the middle age (122.3±1.4)-(121.8±1.3) Ma, and the late age (114.9±1.8) Ma. All three cycles fall into the period of Early Cretaceous. In comparison with the different region in western Liaoning,the volcanic activity of this area occurred in the middle to late cycle according to the chronological characteristics. Yixian Formation in different region of western Liaoning was formed asynchronously, in an extension environment of the related subduction of the Paleo-Pacific plate towards the Eurasian continent.

Key words: Yixian Formation, volcanic rocks, LA-ICP-MS zircon U-Pb dating, the age comparison, Paleo-Pacific plate, western of Liaoning, Jianping Machang

CLC Number: 

  • P588.14

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