青海南山东段花岗岩LA-ICP-MS锆石U-Pb定年及其地质意义

    LA-ICP-MS zircon U-Pb dating of the granites in the eastern section of Nanshan, Qinghai Province, and its geological significance

    • 摘要: 青海南山东段花岗岩类岩石类型为二长花岗岩、花岗闪长岩及英云闪长岩。通过高精度LA-ICP-MS锆石U-Pb同位素测年,获得二长花岗岩、花岗闪长岩的年龄分别为241±3Ma、245±2Ma和249±3Ma,可代表其成岩年龄。花岗岩类构造环境判别图显示,岩石具俯冲型花岗岩类特征,可能代表早三叠世宗务隆洋的北向俯冲过程。通过对青海南山东段侵入岩体形成时代、岩石成因、构造环境等的研究,为青海宗务隆造山带在印支期的构造环境演化和动力学机制提供了重要的依据。

       

      Abstract: The granitic plutons in the eastern section of Nanshan within Qinghai Province consist of monzogranite, granodiorite and tonalite. The zircon U-Pb dating results of monzogranite and granodiorite are 241±3Ma, 245±3Ma and 249±3Ma respectively, representing the crystallization age of those granitoids. In tectonic discrimination diagram for granitic rocks, these samples fall in the subduction field, indicating the north subduction of the Zongwulong oceanic crust in Early Triassic. Through the research on petrogenesis, ages and tectonic setting for granitic plutons in the eastern section of Nanshan within Qinghai Province along Zongwulong belt, this paper provides important evidence for the tectonic environment and geodynamic mechanism of the Zongwulong belt in Early Triassic.

       

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