Detrital zircon U-Pb and Hf isotopic constraints on the crustal evolution of North Korea
文献类型：期刊论文
| 作者 | Wu, Fu-Yuan; Yang, Jin-Hui; Wilde, Simon A.; Liu, Xiao-Ming; Guo, Jing-Hui; Zhai, Ming-Guo |
| 刊名 | PRECAMBRIAN RESEARCH
 |
| 出版日期 | 2007-11-15 |
| 卷号 | 159期号:3-4页码:155-177 |
| 关键词 | crustal evolution Hf isotopes detrital zircon U-Pb dating North Korea |
| ISSN号 | 0301-9268 |
| DOI | 10.1016/j.precamres.2007.06.007 |
| 文献子类 | Article |
| 英文摘要 | The crustal evolution of North Korea is poorly constrained. This study utilises detrital zircon U-Pb and Lu-Hf isotopic data, obtained from sands at the mouths of the Taedong, Chongchon and Songchon Rivers, in order to sample the Rangnim massif. These data are then used to constrain the magmatic age spectrum and crustal growth history of this massif. Zircon U-Pb analyses indicate that the Rangnim Massif, previously considered to be an Archean block, is characterized by similar to 1.8 Ga magmatism, with subsequent peaks at 220 and 110 Ma. Archean magmatism appears to be limited, which is in marked contrast to the nearby North China Craton in terms of the timing of Precambrian events although the oldest age obtained is similar to 3.4 Ga, indicating the existence of some Mesoarchean material in North Korea. In situ zircon Hf isotopic data show that some zircons have Hf model ages up to 4.0 Ga, suggesting a more ancient crustal history. The Hf isotopic data also indicate that the similar to 1.8 Ga zircons have Archean Hf model ages, suggesting derivation from recycled Archean material. Phanerozoic zircons are less abundant than those of Precambrian age, however, the limited data indicate that Phanerozoic magmatism mostly occurred in the Mesozoic, accompanied by significant juvenile crustal growth. The similarities of the crustal formation ages and similar to 1.8 Ga thermal event between the Rangnim Massif and the North China Craton indicate that they were probably a coherent block since Archean time. (c) 2007 Elsevier B.V. All rights reserved. |
| WOS关键词 | PLASMA-MASS SPECTROMETRY ; RAPAKIVI GRANITE BATHOLITH ; SOUTH CHINA COLLISION ; LU-HF ; DABIE-SULU ; SEDIMENTARY PROVENANCE ; TECTONIC CORRELATION ; WESTERN-AUSTRALIA ; GYEONGGI MASSIF ; EASTERN BLOCK |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000250893000002 |
| 出版者 | ELSEVIER SCIENCE BV |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/68620]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Wu, Fu-Yuan |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Curtin Univ Technol, Dept Appl Geol, Perth, WA 6845, Australia 3.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 750069, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wu, Fu-Yuan,Yang, Jin-Hui,Wilde, Simon A.,et al. Detrital zircon U-Pb and Hf isotopic constraints on the crustal evolution of North Korea[J]. PRECAMBRIAN RESEARCH,2007,159(3-4):155-177. |
| APA | Wu, Fu-Yuan,Yang, Jin-Hui,Wilde, Simon A.,Liu, Xiao-Ming,Guo, Jing-Hui,&Zhai, Ming-Guo.(2007).Detrital zircon U-Pb and Hf isotopic constraints on the crustal evolution of North Korea.PRECAMBRIAN RESEARCH,159(3-4),155-177. |
| MLA | Wu, Fu-Yuan,et al."Detrital zircon U-Pb and Hf isotopic constraints on the crustal evolution of North Korea".PRECAMBRIAN RESEARCH 159.3-4(2007):155-177. |
入库方式： OAI收割
来源：地质与地球物理研究所
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