• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    Volume 43 Issue 12
    Dec.  2018
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    Article Contents
    Li Zuochen, Li Ruibao, Pei Lei, Chen Youxin, Liu Chengjun, Pei Xianzhi, Liu Zhanqing, Chen Guochao, Li Xiaobing, 2018. Magmatic Response to Proto-Tethyan Ocean Subduction in East Section of East Kunlun: Evidence from Zircon U-Pb Dating of Late Sinian Dundeshaerguole Hornblende Monzonite. Earth Science, 43(12): 4536-4550. doi: 10.3799/dqkx.2018.173
    Citation: Li Zuochen, Li Ruibao, Pei Lei, Chen Youxin, Liu Chengjun, Pei Xianzhi, Liu Zhanqing, Chen Guochao, Li Xiaobing, 2018. Magmatic Response to Proto-Tethyan Ocean Subduction in East Section of East Kunlun: Evidence from Zircon U-Pb Dating of Late Sinian Dundeshaerguole Hornblende Monzonite. Earth Science, 43(12): 4536-4550. doi: 10.3799/dqkx.2018.173

    Magmatic Response to Proto-Tethyan Ocean Subduction in East Section of East Kunlun: Evidence from Zircon U-Pb Dating of Late Sinian Dundeshaerguole Hornblende Monzonite

    doi: 10.3799/dqkx.2018.173
    • Received Date: 2018-03-23
    • Publish Date: 2018-12-15
    • The study of Neoproterozoic magmatic rocks in the East Kunlun orogenic belt has important significances for the evolution of Proto-Tethys. Taking the Late Sinian Dundeshaerguole hornblende monzonite in east section of East Kunlun as research object, this paper constrains on the Pan-African orogenic events, tension and breach of back-arc basin in East Kunlun and Proto-Tethyan Ocean subduction by the zircon U-Pb dating in combination with regional geological data.The lithological and geochemical data indicate that Dundeshaerguole hornblende monzonite is characterized by potassic alkaline rocks. All the zircons selected from sample 11029/8 have magmatic oscillatory zoning, high Th/U ratios of 0.21-0.41, representing the magmatic origin. The LA-ICP-MS zircon U-Pb dating shows age of 544.8±7.8 Ma (MSWD=5.7), belonging to Ediacaran period in Sinian or Early Cambrian. It is concluded that the Dundeshaerguole hornblende monzonite is the products of northward subduction of Proto-Tethys.

       

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