2.1Ga crustal remelting event in Hengshan Complex: Evidence from zircon U-Pb dating and Hf-Nd isotopic study on potassic granites. | |
Zhao RuiFu; Guo JingHui; Peng Peng; Liu Fu | |
刊名 | ACTA PETROLOGICA SINICA |
2011-06-01 | |
卷号 | 27期号:6页码:1607-1623 |
关键词 | Potassic granite Crustal melting event Paleoproterozoic Hengshan Complex North China Craton |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | The Hengshan Complex in the Central Zone of the North China Craton, which is a typical high-grade terrain and experienced 1.85Ga high-pressure granulite facies metamorphism, composes of similar to 2.5Ga TTG gneisses and some paragneisses. A suite of potassic granites in this complex is investigated, which mainly consists of hornblende monzogranitie and biotite monzogranite. Zircon grains from a hornblende monzogranite sample yield a weighted average (207)Pb/(206)Pb age of 2052 +/- 17Ma by LA-ICP-MS and 2084 +/- 4Ma by SIMS. A biotite monzogranite sample gives a weighted average (207)Pb/(206)Pb age of 2060 +/- 18Ma by LA-ICP-MS and 2083 +/- 15Ma by SIMS. Ca. 2080Ma SIMS ages possibly indicate the crystallization time of these potassic granites. epsilon(Hf)(t) values of zircons in the granites range from -6.0 to 0.6 with t(DM) (depleted mantle model ages) of 2.48 similar to 2.60Ga, while epsilon(Nd)(t) values range from -3.3 to -1.7 with t(DM) of 2.43 similar to 2.68Ga. These indicate that the potassic granites were likely derived from ancient crust. Together with the geochemical characteristics of the surrounding TTG rocks, we suggest that the similar to 2.1Ga potassic granites could be originated from the partial melting of the 2.5Ga TTG gneisses. This study confirms a Paleoproterozoic (similar to 2.1Ga) crust remelting event in Hengshan Complex, which may occur in an extensional setting in the North China Craton. |
WOS关键词 | NORTH CHINA CRATON ; PALEOPROTEROZOIC EVOLUTION ; FUPING COMPLEX ; GEOCHRONOLOGICAL CONSTRAINTS ; ZHONGTIAO MOUNTAINS ; TECTONIC EVOLUTION ; BASEMENT ROCKS ; EASTERN BLOCK ; CENTRAL ZONE ; AGE |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000292995600004 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/74546] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Zhao RuiFu |
作者单位 | Chinese Acad Sci, Stale Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Zhao RuiFu,Guo JingHui,Peng Peng,et al. 2.1Ga crustal remelting event in Hengshan Complex: Evidence from zircon U-Pb dating and Hf-Nd isotopic study on potassic granites.[J]. ACTA PETROLOGICA SINICA,2011,27(6):1607-1623. |
APA | Zhao RuiFu,Guo JingHui,Peng Peng,&Liu Fu.(2011).2.1Ga crustal remelting event in Hengshan Complex: Evidence from zircon U-Pb dating and Hf-Nd isotopic study on potassic granites..ACTA PETROLOGICA SINICA,27(6),1607-1623. |
MLA | Zhao RuiFu,et al."2.1Ga crustal remelting event in Hengshan Complex: Evidence from zircon U-Pb dating and Hf-Nd isotopic study on potassic granites.".ACTA PETROLOGICA SINICA 27.6(2011):1607-1623. |
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