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Chinese Academy of Sciences Institutional Repositories Grid
Late Devonian magmatic event in the South Beishan orogenic belt, Gansu: Constraints from zircon U-Pb chronology, geochemistry and Sr-Nd-Hf isotopes

文献类型:期刊论文

作者Lu Xin1,2; Yu XiaoFei1,2; Du ZeZhong1,2; Kang Kai3; Du YiLun1,2; Wang ChunNu1,2
刊名ACTA PETROLOGICA SINICA
出版日期2022-03-01
卷号38期号:3页码:693-712
关键词Magmatic Event Late Devonian Tectonic setting Beishan Orogenic belt Central Asian Orogenic Belt
ISSN号1000-0569
DOI10.18654/1000-0569/2022.03.07
英文摘要Beishan orogenic belt (BOB) is located on the southern margin of the Central Asian Orogenic Belt (CAOB). The study of magmatic events in BOB is of great significance for understanding the tectonic evolution of the CAOB. A large number of granitiod plutons are distributed in the south of BOB, where the Shuangyingshan and Huaniushan arcs are located. In this study, we focus on granodiorite and monzogranite from the south Shuangfengshan complex in the southern BOB. We present whole rock geochemistry, Sr-Nd isotopic composition, in situ U-Pb dating and Hf isotopic composition of zircons from this complex, from which the following results are obtained : (1) The granodiorites and monzogranites have similar zircon U-Pb chronology, whole rock geochemistry and isotopic composition. (2) Zircon LA-ICP-MS U-Pb dating yields ages of 367. 5 +/- 1. 7Ma and 368.0 +/- 1. 8Ma for the monzogranite, and 366. 3 +/- 2. 2Ma for the granodiorite, suggesting they were formed in the Late Devonian. (3) The SiO2 contents from samples collected in the complex are 64. 39% similar to 74. 95% , with alkali contents of 5. 01% similar to 9. 21% , suggesting it belongs to metaluminous (A/CNK = 0. 88 similar to 1. 00) ; the measured samples have low P2O5, contents (0. 02% similar to 0. 17% ) , which are negatively correlated to SiO2. These features indicated they are of typical I-type granite characteristics. (4) For the REE compositions, this complex is characterized by enriched light rare earth elements ( ( La/Yb)(N) = 6. 23 similar to 23. 0) , negative Eu anomaly (delta Eu = 0. 31 similar to 0. 55) , enriched large ion lithophile elements, such as Rb, Th, U, and depleted high field strength elements such as Nb, Ti, and P. (5) The complex has epsilon(Hf) (t) values of -3. 1 similar to + 6. 0, two stage model ages (t(DM2)) of 928 similar to 1327Ma, (Sr-87/Sr-86), values of 0. 705607 similar to 0. 708523 , and epsilon(Nd) ( t) values of -4. 1 similar to - 1. 9. Combined with the regional geology and tectonic environment, these data reveals that the south Shuangfengshan complex was formed in an active continental margin in Late Devonian, and during its evolution, the lower crust was partially melted by the underplating of mantle-derived magma and mixing with mantle-derived materials, which represented a northward subduction of the Liuyuan Ocean plate in the Late Devonian.
WOS关键词TECTONIC IMPLICATIONS ; DISCRIMINATION ; GEOCHRONOLOGY ; PETROGENESIS ; GRANITES
WOS研究方向Geology
语种英语
WOS记录号WOS:000780616600007
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/105096]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Yu XiaoFei
作者单位1.China Geol Survey, Dev & Res Ctr, Beijing 100037, Peoples R China
2.Minist Nat Resources, Mineral Explorat Tech Guidance Ctr, Beijing 100083, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
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Lu Xin,Yu XiaoFei,Du ZeZhong,et al. Late Devonian magmatic event in the South Beishan orogenic belt, Gansu: Constraints from zircon U-Pb chronology, geochemistry and Sr-Nd-Hf isotopes[J]. ACTA PETROLOGICA SINICA,2022,38(3):693-712.
APA Lu Xin,Yu XiaoFei,Du ZeZhong,Kang Kai,Du YiLun,&Wang ChunNu.(2022).Late Devonian magmatic event in the South Beishan orogenic belt, Gansu: Constraints from zircon U-Pb chronology, geochemistry and Sr-Nd-Hf isotopes.ACTA PETROLOGICA SINICA,38(3),693-712.
MLA Lu Xin,et al."Late Devonian magmatic event in the South Beishan orogenic belt, Gansu: Constraints from zircon U-Pb chronology, geochemistry and Sr-Nd-Hf isotopes".ACTA PETROLOGICA SINICA 38.3(2022):693-712.

入库方式: OAI收割

来源:地质与地球物理研究所

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