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SHRIMP zircon U-Pb age and significance of Early Paleozoic volcanic rocks in East Kunlun orogenic belt, Qinghai Province, China

机译:青海省东昆仑造山带的SHRIMP锆石U-Pb年龄和早期古生代火山岩的意义

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摘要

Early Paleozoic volcanic rocks in Nuomuhong area occurred as basalt slice and meta-volcanic slice. SHRIMP zircon U-Pb dating of the basalt slice and the meta-volcanic slice show that the age of the basalt slice is 419 ± 5 Ma, and that of the meta-volcanic slice is 401 ± 6 Ma. These ages directly testify that there existed Early Paleozoic ocean-continent transform in East Kunlun, the basalt slice was formed in an extensional mid-ocean ridge setting and the meta-volcanic rock slice was formed in an extrusion subduction and collision setting. The inherited zircon age of 1734 Ma in volcanic rocks reflects that the base of East Kunlun may be Middle Proterozoic.
机译:糯木洪地区早古生代火山岩为玄武岩片和中火山岩片。玄武岩片和准火山岩片的SHRIMP锆石U-Pb测年表明玄武岩片的年龄为419±5 Ma,准火山岩的年龄为401±6 Ma。这些年龄直接证明了东昆仑存在早古生代海陆转换,玄武岩片形成于伸展的中海脊背景,而超火山岩片则形成于挤压俯冲和碰撞环境。火山岩中1734 Ma的锆石遗传年龄反映出东昆仑的基底可能是中元古代。

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