中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Petrogenesis and tectonic setting of 2. 2 similar to 2. 1 Ga granites in Wutai area, North China Craton

文献类型:期刊论文

作者Du LiLin1; Yang ChongHui1; Song HuiXia1; Zhao Lei2; Lu ZengLong1; Li Lun1,3; Wang Tao1; Ren LiuDong1
刊名ACTA PETROLOGICA SINICA
出版日期2018
卷号34期号:4页码:1154-+
关键词2. 2Ga to 2. 1Ga granites Zircon U-Pb age Geochemistry Zircon Hf isotope Intracontinental rift Wutai area
ISSN号1000-0569
文献子类Article
英文摘要2. 2 similar to 2. 0Ga magmatism widely occurs in the Trans-North China Orogen (TNCO), which is vital for unveiling the Paleoproterozoic tectonic evolution on the North China Craton (NCC). This paper presents the whole rock geochemical data, zircon U-Pb ages and Hf isotopes of Paleoproterozoic Dawaliang, Wangjiahui and Lianhuashan granitoids in Wutai area. SHRIMP U-Pb zircon dating of Dawaliang porphyritic granite sample yields an age of 2170 +/- 17Ma. One sample from Wangjiahui monzonitic granitic gneiss obtains a LA-ICPMS zircon U-Pb age of 2101 +/- 6Ma, and 3 samples from Lianhuashan granite gets zircon U-Pb ages of 2117 +/- 6Ma, 2110 +/- 4Ma and 2143 +/- 15Ma, respectively. Dawaliang granite is high in SiO2 and K2O +Na2O, low in CaO, and enriched in REEs (except Eu), Zr, Nb, Ga and Y, and depleted in Sr. Meanwhile, all samples of Dawaliang granite have high Ga/Al values and Zr + Nb + Y + Ce contents with whole rock zircon saturation temperature as high as 876 similar to 986 degrees C, which is identical with the features of the A-type granite. Wangjiahui and Lianhuashan granites enrich in SiO2, K2O and Na2O, and deplete in MgO and CaO, on the other hand, the granites show minor to intensive differentiation on REEs with obviously negative Eu abnormity. Three plutons (Dawaliang, Wangjiahui and Lianhuashan granites) have high Nb and Y concentrations, so they show the features of post-collision and within plate granite. Zircon epsilon(Hf)(t) values in all samples are lower than that in depleted mantle, and meanwhile, one and two stage Hf model ages are 2. 4 similar to 2. 6Ga and 2. 45 similar to 2. 75Ga, respectively, which are much older than the zircon U-Pb ages of the granites. Combining petrology, geochemistry and isotope in the samples, we propose that the Paleoproterozoic granites are derived from the partial melting by the Late Archean TTG gneisses under the extensional environment. Considering the 2. 2 similar to 2. 0Ga magmatism along the TNCO exhibits two stages of 2. 2 similar to 2. 1Ga and 2. 1 similar to 2. 0Ga in different regions, in which 2. 2 similar to 2. 1 Ga magma represent the early stage and some granites at this stage show the features of A-type granite and form the bimodal magmatic assemblages with the coeval mafic rocks. Therefore, we deduce that the middle of Paleoproterozoic magmatism is related with the intracontinental rift in the NCC.
WOS关键词ZIRCON U-PB ; A-TYPE GRANITES ; GRANULITIC METASEDIMENTARY ROCKS ; PALEOPROTEROZOIC HUTUO GROUP ; PLASMA-MASS SPECTROMETRY ; HIGH-PRESSURE GRANULITES ; HF ISOTOPIC EVIDENCE ; CRUSTAL EVOLUTION ; ZANHUANG COMPLEX ; LASER-ABLATION
WOS研究方向Geology
语种英语
WOS记录号WOS:000431895400016
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/88282]  
专题中国科学院地质与地球物理研究所
通讯作者Du LiLin
作者单位1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
推荐引用方式
GB/T 7714
Du LiLin,Yang ChongHui,Song HuiXia,et al. Petrogenesis and tectonic setting of 2. 2 similar to 2. 1 Ga granites in Wutai area, North China Craton[J]. ACTA PETROLOGICA SINICA,2018,34(4):1154-+.
APA Du LiLin.,Yang ChongHui.,Song HuiXia.,Zhao Lei.,Lu ZengLong.,...&Ren LiuDong.(2018).Petrogenesis and tectonic setting of 2. 2 similar to 2. 1 Ga granites in Wutai area, North China Craton.ACTA PETROLOGICA SINICA,34(4),1154-+.
MLA Du LiLin,et al."Petrogenesis and tectonic setting of 2. 2 similar to 2. 1 Ga granites in Wutai area, North China Craton".ACTA PETROLOGICA SINICA 34.4(2018):1154-+.

入库方式: OAI收割

来源:地质与地球物理研究所

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