Contrasting source domains for the Phanerozoic granitoids in South Korea revealed by zircon Hf isotopic signatures
文献类型：期刊论文
| 作者 | Lee, Seung Ryeol1; Cho, Deung-Lyong1; Wu, Fu-Yuan2 |
| 刊名 | GEOSCIENCES JOURNAL
 |
| 出版日期 | 2016-10-01 |
| 卷号 | 20期号:5页码:585-596 |
| 关键词 | Korean Peninsula Zircon Hf Isotope Phanerozoic Granitoids Precambrian Basement Subduction-related Magmatism |
| DOI | 10.1007/s12303-016-0028-7 |
| 文献子类 | Article |
| 英文摘要 | In situ zircon Hf isotopic analysis was conducted to investigate the characteristics of source materials responsible for generations of the Phanerozoic granitoids in South Korea. The Hf isotopic data compiled from the literature together with this study revealed two principal types of source materials governing the generation of the Permo-Triassic granitoids. One type corresponds to long-lasting, ancient lithospheric materials having highly negative EEO values of 24.3 to 18.6 and is temporally equivalent to the Paleoproterozoic to Neoarchean basement rocks prevalent in South Korea. This type is a primary source material for the Triassic postorogenic granitoids in the Gyeonggi massif The other type corresponds to juvenile materials accreted by Late Paleozoic continental arc magmatism. This relatively young crust occurs largely in and around the Gyeongsang basin. Systematic southeastward increase in epsilon Hf(t) values of both Permo-Triassic and Jurassic granitoids indicates enhanced contributions of juvenile materials toward the paleo-trench. Such a trend is best explained by the chemical mixing of two principal types of source. Northern limit of chemical interactions between ancient and juvenile components is inferred to lie along the central Okcheon belt during the Permo-Triassic. However, this boundary has shifted southeastward in Jurassic to be defined by the Sunchang Yecheon shear zone, a part of the Honam Shear Zone. The arc-related juvenile crust was also a principal source for the Cretaceous-Paleogene granitoids in the Gyeongsang basin. |
| WOS关键词 | NEOPROTEROZOIC BIMODAL VOLCANISM ; NORTHEASTERN YEONGNAM MASSIF ; U-PB AGES ; TECTONIC IMPLICATIONS ; CRUSTAL EVOLUTION ; GYEONGGI MASSIF ; ARC MAGMATISM ; OGCHEON BELT ; LU-HF ; INDOSINIAN OROGENY |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000384518800001 |
| 资助机构 | Basic Research Program of Korea Institute of Geoscience and Mineral Resources (KIGAM)(15-3116) ; Basic Research Program of Korea Institute of Geoscience and Mineral Resources (KIGAM)(15-3116) ; Basic Research Program of Korea Institute of Geoscience and Mineral Resources (KIGAM)(15-3116) ; Basic Research Program of Korea Institute of Geoscience and Mineral Resources (KIGAM)(15-3116) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/53342]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 作者单位 | 1.Korea Inst Geosci & Mineral Resources, Div Geol Res, Daejeon 34132, South Korea 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithosphere Evolut, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Lee, Seung Ryeol,Cho, Deung-Lyong,Wu, Fu-Yuan. Contrasting source domains for the Phanerozoic granitoids in South Korea revealed by zircon Hf isotopic signatures[J]. GEOSCIENCES JOURNAL,2016,20(5):585-596. |
| APA | Lee, Seung Ryeol,Cho, Deung-Lyong,&Wu, Fu-Yuan.(2016).Contrasting source domains for the Phanerozoic granitoids in South Korea revealed by zircon Hf isotopic signatures.GEOSCIENCES JOURNAL,20(5),585-596. |
| MLA | Lee, Seung Ryeol,et al."Contrasting source domains for the Phanerozoic granitoids in South Korea revealed by zircon Hf isotopic signatures".GEOSCIENCES JOURNAL 20.5(2016):585-596. |
入库方式： OAI收割
来源：地质与地球物理研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。