中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Application of the revised Ti-in-zircon thermometer and SIMS zircon U-Pb dating of high-pressure pelitic granulites from the Qianlishan-Helanshan Complex of the Khondalite Belt, North China Craton

文献类型:期刊论文

作者Qiao, Hengzhong1,2; Yin, Changqing1,2; Li, Qiuli3; He, Xiaolan1,2; Qian, Jiahui1,2; Li, Wenjing1,2
刊名PRECAMBRIAN RESEARCH
出版日期2016-05-01
卷号276页码:1-13
关键词Ti-in-zircon Thermometer Sims U-pb Dating Pelitic Granulites Paleoproterozoic Khondalite Belt
DOI10.1016/j.precamres.2016.01.020
文献子类Article
英文摘要The Ti-in-zircon thermometer is a newly established, single-mineral trace element thermometer, which has been successfully used to estimate the peak and post-peak temperatures of high-grade metamorphic rocks. Here the revised Ti-in-zircon thermometer and in situ SIMS U-Pb dating are applied to detrital and metamorphic zircons of pelitic granulites from the Qianlishan-Helanshan Complex. The SIMS U-Pb results show that detrital zircons yield Pb-207/Pb-206 ages scattering from 2021 to 2449 Ma with a peak age of 2030 Ma, possibly sourced from felsic to intermediate igneous rocks at a relatively low temperature magmatic environment. Most metamorphic zircons yield ages of 1953 +/- 15 Ma, 1954 +/- 20 Ma and 1948 +/- 18 Ma with Ti contents of 3.9-82.6 ppm, corresponding to metamorphic temperatures of 664-992 degrees C. Minor metamorphic zircons give Pb-207/Pb-206 ages of 1923 +/- 9 Ma and Ti contents of 5.8-16.3 ppm with temperatures of 697-794 degrees C. These define metamorphic ages and temperature conditions at peak and post-peak metamorphic stages of pelitic granulites, respectively. Combined with previous studies, our new data establish a linking between zircon U-Pb ages and metamorphic thermal evolution. This demonstrates a similar to 1.95 Ga peak temperature granulite-facies metamorphism and subsequent near-isothermal decompression process at similar to 1.92 Ga, which is considered to record a similar to 1.95 Ga continent-continent collisional event between the Yinshan and Ordos blocks, followed by post-orogenic exhumation at similar to 1.92 Ga. (C) 2016 Elsevier B.V. All rights reserved.
WOS关键词ULTRAHIGH-TEMPERATURE METAMORPHISM ; WESTERN BLOCK ; KEY ISSUES ; ICP-MS ; TECTONIC IMPLICATIONS ; CRUSTAL METAMORPHISM ; RUTILE THERMOMETERS ; DETRITAL ZIRCONS ; JINING COMPLEX ; EVOLUTION
WOS研究方向Geology
语种英语
WOS记录号WOS:000373866300001
资助机构Chinese 1000 Young Talents Program, Chinese NSFC Grants(41190075 ; Chinese 1000 Young Talents Program, Chinese NSFC Grants(41190075 ; Hong Kong RGC(7069/12P) ; Hong Kong RGC(7069/12P) ; 40730315 ; 40730315 ; 40872123) ; 40872123) ; Chinese 1000 Young Talents Program, Chinese NSFC Grants(41190075 ; Chinese 1000 Young Talents Program, Chinese NSFC Grants(41190075 ; Hong Kong RGC(7069/12P) ; Hong Kong RGC(7069/12P) ; 40730315 ; 40730315 ; 40872123) ; 40872123)
源URL[http://ir.iggcas.ac.cn/handle/132A11/53454]  
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.Sun Yat Sen Univ, Sch Earth Sci & Geol Engn, Guangzhou 510275, Guangdong, Peoples R China
2.Sun Yat Sen Univ, Guangdong Prov Key Lab Mineral Resources & Geol P, Guangzhou 510275, Guangdong, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Qiao, Hengzhong,Yin, Changqing,Li, Qiuli,et al. Application of the revised Ti-in-zircon thermometer and SIMS zircon U-Pb dating of high-pressure pelitic granulites from the Qianlishan-Helanshan Complex of the Khondalite Belt, North China Craton[J]. PRECAMBRIAN RESEARCH,2016,276:1-13.
APA Qiao, Hengzhong,Yin, Changqing,Li, Qiuli,He, Xiaolan,Qian, Jiahui,&Li, Wenjing.(2016).Application of the revised Ti-in-zircon thermometer and SIMS zircon U-Pb dating of high-pressure pelitic granulites from the Qianlishan-Helanshan Complex of the Khondalite Belt, North China Craton.PRECAMBRIAN RESEARCH,276,1-13.
MLA Qiao, Hengzhong,et al."Application of the revised Ti-in-zircon thermometer and SIMS zircon U-Pb dating of high-pressure pelitic granulites from the Qianlishan-Helanshan Complex of the Khondalite Belt, North China Craton".PRECAMBRIAN RESEARCH 276(2016):1-13.

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来源:地质与地球物理研究所

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