长江现代沉积物碎屑锆石U-Pb年龄及Hf同位素组成与物源示踪研究
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摘要
为研究长江沉积物物质来源,对长江流域24个现代沉积物样品进行碎屑锆石U-Pb年龄测试,并对10个样品做Hf同位素分析,结果表明:长江河流沉积物的碎屑锆石多为岩浆成因。碎屑锆石U-Pb年龄主要有6组峰:2.4~2.6Ga,1.8~2.0Ga,700~1000Ma,400~550Ma,200~300Ma和<65Ma,其中200~300Ma和700~1000Ma为主要的两组峰。锆石U-Pb年龄谱系可区分出长江4个区段,即金沙江段、川江段、长江中游段和下游段,与地理分段相吻合。结合Hf同位素研究,可认为长江流域沉积物中生代-新生代的锆石主要来自松潘-甘孜褶皱带和秦岭造山带;古生代的锆石多来自秦岭造山带;元古代-太古代的锆石则多来自扬子克拉通、华夏地块和大别造山带。
A total of 24 sand samples were collected in the mainstream and major tributaries of the Yangtze River drainage basin.The sample sites include the whole drainage,from the source "Tuotuohe" to the river mouth.Three samples were taken at the confluence of the mainstream and tributaries,avoiding potential contaminates.24 samples were dated by the LA-ICP-MS U-Pb technique and 10 samples were analyzed for Hf isotopes on the same spots of concordant grains.Our results show that most zircons are from igneous rocks,so the ages of these zircons could represent the time of their crystallization.The U-Pb age specturm define six age groups in mainstream of the Jinshajiang;2.4~2.6Ga,1.8 ~ 2.OGa,700 ~ 1000Ma,400 ~550Ma,200 ~ 300Ma and <65Ma(Fig.7A ~ 7D),and two in the tributaries:700 ~ 900Ma and 100 ~300Ma(Fig.8A ~8D).There are four age groups in the Chuanjiang:2.4 ~ 2.6Ga,1.8 ~ 2.OGa,700 ~lOOOMa and 200 ~ 300Ma(Fig.7E ~ 7G,Fig.8E ~ 8F).Among which,2.4-2.6Ga are enrichment in the Jialingjiang and Wujiang.Five age groups display in the mainstream of the Midstream:2.4-2.6Ga,l.8 ~2.OGa,700 ~ 1000Ma,400 ~500Ma and 200 ~ 300Ma(Fig.7H- 7K).whereas
A total of 24 sand samples were collected in the mainstream and major tributaries of the Yangtze River drainage basin.The sample sites include the whole drainage,from the source "Tuotuohe" to the river mouth.Three samples were taken at the confluence of the mainstream and tributaries,avoiding potential contaminates.24 samples were dated by the LA-ICP-MS U-Pb technique and 10 samples were analyzed for Hf isotopes on the same spots of concordant grains.Our results show that most zircons are from igneous rocks,so the ages of these zircons could represent the time of their crystallization.The U-Pb age specturm define six age groups in mainstream of the Jinshajiang;2.4~2.6Ga,1.8 ~ 2.OGa,700 ~ 1000Ma,400 ~550Ma,200 ~ 300Ma and <65Ma(Fig.7A ~ 7D),and two in the tributaries:700 ~ 900Ma and 100 ~300Ma(Fig.8A ~8D).There are four age groups in the Chuanjiang:2.4 ~ 2.6Ga,1.8 ~ 2.OGa,700 ~lOOOMa and 200 ~ 300Ma(Fig.7E ~ 7G,Fig.8E ~ 8F).Among which,2.4-2.6Ga are enrichment in the Jialingjiang and Wujiang.Five age groups display in the mainstream of the Midstream:2.4-2.6Ga,l.8 ~2.OGa,700 ~ 1000Ma,400 ~500Ma and 200 ~ 300Ma(Fig.7H- 7K).whereas
引文
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4王中波,杨守业,王汝成等.长江河流沉积物磁铁矿化学组成及其物源示踪.地球化学,2007,36(2):176-184Wang Zhongbo,Yang Shouye,Wang Rucheng et al.Magnetite compositions of Changjiang River sediments and their tracing implications.Geochimica,2007,36(2):176-184
5 He Mengying,Zheng Hongbo,Huang Xiangtong et al.Yangtze River sediments from source to sink traced with clay mineralogy.Journal of Asian Earth Sciences,2013(in press)
6 Kent C Condie,Eloise Beyer,Elena Belousova et al.U-Pb isotopic ages and Hf isotopic composition of single zircons;The search for juvenile Precambrian continental crust.Precambrian Research,2005,139(1-2):42-100
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8 Tsuyoshi Lizuka,Takafumi Hirata,Tsuyoshi Komiya et al.U-Pb and Lu-Hf isotope systematics of zircons from the Mississippi River sand:Implications for reworking and growth of continental crust.Geology,2005,33(6):485-488
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