Petrogenesis of typical Mesozoic and Cenozoic volcanic rocks from the North China Craton: new evidence from Hf isotopic studies | |
Yang YueHeng; Zhang HongFu; Xie LieWen; Liu Ying; Qi ChangShi; Tu XiangLin | |
刊名 | ACTA PETROLOGICA SINICA
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2006-06-01 | |
卷号 | 22期号:6页码:1665-1671 |
关键词 | Hf isotope Mesozoic Cenozoic volcanic rocks petrogenesis |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | High precision Hf isotopic data are firstly reported for the typical Mesozoic and Cenozoic volcanic rocks (alkaline basalts, tholeiites. and high-Mg andesites) from the North China Craton in this paper. The results show that these Mesozoic and Cenozoic volcanic rocks have completely different Hf isotopic compositions with a large range in epsilon(Hf) (t) values (-18.4 similar to 9. 6) with an excellently positive correlation between Hf and Nd isotopes. Among them, the Cenozoic Changle-Linqu and Late Cretaceous Jianguo (similar to 105 Ma) alkaline basalts possess very high Hf and Nd isotopic compositions (epsilon(Hf) (t) = 6.8 similar to 9.6; epsilon(Nd) (t) = 0.4 similar to 4. 9), indicating their derivation from the undifferentiated asthenospheric source. Early Cretaceous Fangcheng (125Ma) alkaline basalts and tholeiites have extremely low Hf and Nd isotopic ratios (epsilon(Hf)(t) = -15.6 similar to -18.4; epsilon(Nd) (t) = -12.8 similar to -14.4), representing their origination from an enriched sub-continental lithospheric mantle. Wulahada (142Ma) high-Mg andesites show relatively lower Hf and Nd isotopic ratios (epsilon(Hf)(t) = -2.1 similar to -2.6), implying a derivation from old refractory lithospheric mantle contaminated with melt fulid released from subducted crustal materials. Relatively larger variations in Hf isotopic compositions of basalts (epsilon(Hf) (t)/epsilon(Nd) (t) > 1 demonstrate that the Hf isotopes could be better tracer of mantle sources than the Nd isotopes. |
WOS关键词 | LITHOSPHERIC MANTLE ; CHEMICAL-SEPARATION ; TECTONIC EVOLUTION ; LU-HF ; ND ; BASALTS ; BENEATH ; ICPMS ; SM |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000239220800023 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/67038] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Yang YueHeng |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China 3.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Isotope Geochronol & Geochem, Guangzhou 510640, Peoples R China |
推荐引用方式 GB/T 7714 | Yang YueHeng,Zhang HongFu,Xie LieWen,et al. Petrogenesis of typical Mesozoic and Cenozoic volcanic rocks from the North China Craton: new evidence from Hf isotopic studies[J]. ACTA PETROLOGICA SINICA,2006,22(6):1665-1671. |
APA | Yang YueHeng,Zhang HongFu,Xie LieWen,Liu Ying,Qi ChangShi,&Tu XiangLin.(2006).Petrogenesis of typical Mesozoic and Cenozoic volcanic rocks from the North China Craton: new evidence from Hf isotopic studies.ACTA PETROLOGICA SINICA,22(6),1665-1671. |
MLA | Yang YueHeng,et al."Petrogenesis of typical Mesozoic and Cenozoic volcanic rocks from the North China Craton: new evidence from Hf isotopic studies".ACTA PETROLOGICA SINICA 22.6(2006):1665-1671. |
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