Petrogenesis of similar to 2.1 Ga mafic and granitic magmatism and tectonic implication of Jiaobei Terrane in North China Craton
文献类型：期刊论文
| 作者 | Wang, Xinping1,3; Oh, Chang Whan1; Peng, Peng2 ; Zhao, Lei2; Zhai, Mingguo2; Lee, Seung Hwan1
|
| 刊名 | LITHOS
 |
| 出版日期 | 2020-12-15 |
| 卷号 | 378页码:19 |
| 关键词 | North China Craton Jiao-Liao-Ji belt Jiaobei Terrane Paleoproterozoic magmatism Back-arc basin |
| ISSN号 | 0024-4937 |
| DOI | 10.1016/j.lithos.2020.105806 |
| 英文摘要 | Paleoproterozoic magmatism in the Jiaobei Terrane has not been well studied, but it is important for understanding the tectonic evolution of Jiao-Liao-Ji belt in the east North China Craton. In this work, similar to 2.1 Ga mafic and granitic intrusions in the Jiaobei Terrane, including the Xiliu amphibolite, Dongbaishishan granite and Gujiacun granite, are studied in detail. The Xiliu amphibolite intruded the Archean basement and the Dongbaishishan granite intruded the Paleoproterozoic Jingshan Group. SHRIMP zircon U-Pb geochronology shows that both amphibolite and granite were emplaced simultaneously at similar to 2.1 Ga and were metamorphosed at similar to 1.87-1.84 Ga. The similar to 2.1 Ga Xiliu amphibolite samples show a tholeiitic basalt composition; they exhibit enriched light rare earth elements (REEs) and large ion lithophile elements (LILEs, e.g., U and K), but depleted high field strength elements (HFSEs, e.g., Nb, Ta, P, Zr, Hf and Ti). They experienced the fractional crystallization of clinopyroxene. Whole-rock Nd isotopes show that the similar to 2.1 Ga amphibolites were generated from partial melting of the Archean enriched mantle, and that the mantle source was affected by the addition of subduction-related fluids/melts. The similar to 2.1 Ga Dongbaishishan and Gujiacun granite samples in the Jiaobei Terrane show granodiorite to granite compositions with metaluminous and calc-alkaline characteristics. They show decreasing Fe2O3T, TiO2, Al2O3, CaO, Na2O and P2O5, but increasing K2O, with increasing SiO2 contents. This indicates that Fe-Ti oxide, plagioclase and apatite were fractionated during magmatic evolution, which is confirmed by the negative Eu, Sr, P, and Ti anomalies. Compared with the 2.18 Ga A-type granites derived from partial melting of tonalites in the Jiaobei Terrane, major elemental geochemistry and zircon Hf isotopes showed that similar to 2.1 Ga granites were generated from partial melting of the low-K mafic lower crust possibly due to mantle-derived magmatic underplating. The similar to 2.1 Ga Jiaobei amphibolites show similar geochemical and isotopic characteristics to the contemporaneous mafic rocks in the north Liaoji and south Anhui areas of the Jiao-Liao-Ji belt. Together with the volcano-sedimentary series and A(2)- and I-type granitic gneiss in the belt, these similar to 2.1 Ga mafic rocks probably formed in a subduction-related back-arc extension environment. In addition, both episodes of the 2.18 Ga and 2.1 Ga granites in the Jiaobei Terrane show high-temperature magmatic characters, which can be attributed to mantle-derived magmatic heating. The younger episode (2.1 Ga) granites indicate that there was stronger mantle-derived magmatism in a back-arc extended zone. (C) 2020 Elsevier B.V. All rights reserved. |
| 资助项目 | National Research Foundation of Korea[NRF-2017R1A2B2011224] ; National Research Foundation of Korea[NRF-2017K1A1A201380] ; Chinese Academy of Sciences[132A11KYSB20180042] ; National Natural Science Foundation of China[NSFC-41890833] ; National Natural Science Foundation of China[NSFC-41772192] |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
| 语种 | 英语 |
| WOS记录号 | WOS:000598169500004 |
| 出版者 | ELSEVIER |
| 资助机构 | National Research Foundation of Korea ; National Research Foundation of Korea ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Research Foundation of Korea ; National Research Foundation of Korea ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Research Foundation of Korea ; National Research Foundation of Korea ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Research Foundation of Korea ; National Research Foundation of Korea ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/99935]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 通讯作者 | Wang, Xinping; Oh, Chang Whan |
| 作者单位 | 1.Jeonbuk Natl Univ, Dept Earth & Environm Sci, Jeonju 54896, South Korea 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 3.Shanxi Normal Univ, Sch Geog Sci, Linfen 041000, Shanxi, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Xinping,Oh, Chang Whan,Peng, Peng,et al. Petrogenesis of similar to 2.1 Ga mafic and granitic magmatism and tectonic implication of Jiaobei Terrane in North China Craton[J]. LITHOS,2020,378:19. |
| APA | Wang, Xinping,Oh, Chang Whan,Peng, Peng,Zhao, Lei,Zhai, Mingguo,&Lee, Seung Hwan.(2020).Petrogenesis of similar to 2.1 Ga mafic and granitic magmatism and tectonic implication of Jiaobei Terrane in North China Craton.LITHOS,378,19. |
| MLA | Wang, Xinping,et al."Petrogenesis of similar to 2.1 Ga mafic and granitic magmatism and tectonic implication of Jiaobei Terrane in North China Craton".LITHOS 378(2020):19. |
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。