New Evidence of Detrital Zircon Ages for the Final Closure Time of the Paleo-Asian Ocean in the East

• 作 者: DU Qingxiang HAN Zuozhen SHEN
• 机 构: CollegeofEarthScienceandEngineering,ShandongProvincialKeyLabofDepositionalMineralizationandSedimenta
• 出 处: 地质学报：英文版
• 发表日期: 2017年5期
• 关键词: 中亚造山带 闭合时间 古亚洲洋 锆石年龄 东北 中国 证据 碎屑
• 基金项目: This study was supported by the National Natural ScienceFoundationofChina（grantsNo.41372108and 41602110）,the ResearchFundforthe Doctoral Program ofHigher Education ofChina （grant No. 20133718130001）,

<正>Objective The NE China is located in the eastern segment of the Central Asian Orogenic Belt(CAOB),which is a large accretionary orogen between the Siberian Craton and the North China Craton(NCC).Many researches have discussed about the evolution