Zircon U-Pb ages of Paleoproterozoic mafic granulites from the Huai'an terrane, North China Craton (NCC): Implications for timing of cratonization and crustal evolution history
文献类型：期刊论文
| 作者 | Zhang, Hua-Feng1; Wang, Hao-Zheng2; Santosh, M.1,3; Zhai, Ming-Guo2,4 |
| 刊名 | PRECAMBRIAN RESEARCH
 |
| 出版日期 | 2016 |
| 卷号 | 272页码:244-263 |
| 关键词 | High-pressure granulite Paleoproterozoic Zircon U-Pb dating Huai'an terrane North China Craton |
| DOI | 10.1016/j.precamres.2015.11.004 |
| 文献子类 | Article |
| 英文摘要 | The North China Craton (NCC) is considered to have been incorporated into the Columbia supercontinent during late Paleoproterozoic. The Huai'an terrane located in north-central part of the NCC is an important tectonic window to investigate the Paleoproterozoic crustal evolution history of this craton, particularly due to the wide occurrence of high-grade metamorphic rocks including retrograded eclogites and high-pressure granulites. Available data show two controversial peak metamorphic ages of these rocks as 1.95-1.90 or similar to 4.85-1.80 Ga. Thus, determining the precise timing of metamorphism of the high-pressure granulites is important in reconstructing the collisional history. In this study, we present zircon U-Pb ages, bulk chemistry, and mineral inclusions in zircons and matrix mineral assemblages from the high-pressure granulites to evaluate the timing of metamorphism. Our results reveal ca. 2.05-2.0 Ga ages from magmatic zircons in these rocks representing the timing of emplacement of mafic magmas. The metamorphic zircons yield two groups of ages at 1.95-1.90 and similar to 1.85-1.80 Ga. Clinopyroxene, plagioclase, titanite, and apatite occur as common mineral inclusions within the similar to 1.85-1.80 Ga metamorphic zircons. The chemical compositions of clinopyroxene and plagioclase occurring as inclusions are very similar to those of the rim compositions of those minerals in the matrix, suggesting their formation during retrograde granulite metamorphism, and are distinctly different from those of the core domains of the minerals in the matrix which represent high-pressure granulite metamorphism. These results indicate that the metamorphic zircons formed during retrograde granulite metamorphism dated as similar to 1.85-1.80 Ga and the age range of similar to 1.95-1.90 Ga corresponds to high-pressure granulite metamorphism. The dual nature of the geological and geochronological features suggest that the Archean gray gneisses in the Huai'an terrane represent the basement rocks detached from the Khondalite Belt of the NCC after collision. Integrating with published data, a double-side collision with scissor-like suturing model is proposed for the Paleoproterozoic cratonization of the NCC. (C) 2015 Published by Elsevier B.V. |
| WOS关键词 | HIGH-GRADE METAMORPHISM ; ULTRAHIGH-TEMPERATURE METAMORPHISM ; HIGH-PRESSURE METAMORPHISM ; TRACE-ELEMENT GEOCHEMISTRY ; PRE-RODINIA SUPERCONTINENT ; HF ISOTOPIC EVIDENCE ; S-TYPE GRANITES ; T-T PATHS ; KHONDALITE BELT ; TECTONIC EVOLUTION |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000368868900014 |
| 资助机构 | 973 program(2012CB416603) ; 973 program(2012CB416603) ; Natural Science Foundation of China(41030316) ; Natural Science Foundation of China(41030316) ; Fundamental Research Funds for the Central Universities(53200959742) ; Fundamental Research Funds for the Central Universities(53200959742) ; 973 program(2012CB416603) ; 973 program(2012CB416603) ; Natural Science Foundation of China(41030316) ; Natural Science Foundation of China(41030316) ; Fundamental Research Funds for the Central Universities(53200959742) ; Fundamental Research Funds for the Central Universities(53200959742) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/62074]  |
| 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.China Univ Geosci, Dept Geosci & Resources, Beijing 100083, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Lithospher Evolut, POB 9825, Beijing 100029, Peoples R China 3.Kochi Univ, Fac Sci, Dept Nat Environm Sci, Akebono Cho 2-5-1, Kochi 7808520, Japan 4.NW Univ Xian, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Hua-Feng,Wang, Hao-Zheng,Santosh, M.,et al. Zircon U-Pb ages of Paleoproterozoic mafic granulites from the Huai'an terrane, North China Craton (NCC): Implications for timing of cratonization and crustal evolution history[J]. PRECAMBRIAN RESEARCH,2016,272:244-263. |
| APA | Zhang, Hua-Feng,Wang, Hao-Zheng,Santosh, M.,&Zhai, Ming-Guo.(2016).Zircon U-Pb ages of Paleoproterozoic mafic granulites from the Huai'an terrane, North China Craton (NCC): Implications for timing of cratonization and crustal evolution history.PRECAMBRIAN RESEARCH,272,244-263. |
| MLA | Zhang, Hua-Feng,et al."Zircon U-Pb ages of Paleoproterozoic mafic granulites from the Huai'an terrane, North China Craton (NCC): Implications for timing of cratonization and crustal evolution history".PRECAMBRIAN RESEARCH 272(2016):244-263. |
入库方式： OAI收割
来源：地质与地球物理研究所
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