Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (2): 497-510.doi: 10.13278/j.cnki.jjuese.201702114

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Discovery of the Late Archean Supracrustal Rock to the North of Qinghe Fault in Liaoning Province and Its Geological Significance

Liu Jin1,2, Liu Zhenghong1, Zhao Chen2, Peng Youbo2, Wang Chujie3, Yang Zhongjie2, Dou Shiyong2   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Geological Survey Institute of Liaoning Province, Shenyang 110031, China;
    3. Liaoning Colored Geology Bureau of 108 Team, Shenyang 110031, China
  • Received:2016-06-21 Online:2017-03-26 Published:2017-03-26
  • Supported by:
    Supported by Project of China Geological Survey(12120113057900)

Abstract: By detailed geological mapping in Kaiyuan area, Late Archean supracrustal rocks have been discovered for the first time in the north of the Qinghe fault, which are mainly composed of amphibolite, hornblende-plagioclase leptynite, hornblende-biotite-plagioclase gneiss and hornblendite. Geochemical characteristics of these rocks indicate that their metamorphic original rocks were intermediate or intermediate-basic volcanic rocks which formed in the island arc environment. Such metamorphic structural styles as penetrative schistosity, boudin structure, metamorphic differentiation strip and ptygma fold are commonly found in these metamorphic supracrustal rocks. LA-ICP-MS zircon U-Pb dating of the amphibolite show that these newly discovered Late Archean supracrustal rocks were formed at 2 524±18 Ma and metamorphosed at 2 477±21 Ma.The time interval between emplacement and metamorphism is about 47 Ma. These Late Archean supracrustal rocks confirm that the Archean crystalline basement once existed to the north of the Qinghe fault, and that the structural environment between the Qinghe fault and the Kouhe fault was actually the Late Archean greenstone belt, the same as the Qingyuan area.

Key words: LA-ICP-MS zircon U-Pb dating, northern margin of North China plate, Qinghe fault, Late Archean supracrustal rock, Hongtoushan rock group, geochemistry

CLC Number: 

  • P588.3
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