中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Erroneous determination of the duration of metamorphism from analysis of overlapping pre-sputtered areas during SIMS U?Pb dating of zircon

文献类型:期刊论文

作者Tang, Hu2,3,4; Li, Qiuli2,3,4; Liu, Yu2,4; Shi, Yonghong1
刊名CHEMICAL GEOLOGY
出版日期2021-07-05
卷号573页码:11
关键词Metamorphic zircon SIMS Overlapping pre-sputtered areas Age deviation U?Pb dating
ISSN号0009-2541
DOI10.1016/j.chemgeo.2021.120177
英文摘要The duration of geological events has distinct implications for geological processes. Secondary ion mass spectrometry (SIMS) U?Pb dating of inherited zircon cores and metamorphic rims is the most common method used to determine the age of a protolith, and the timing and duration of metamorphism. This study investigates the age deviation induced by overlapping pre-sputtered areas during SIMS zircon core?rim U?Pb dating, using eclogite and country-rock granitic gneiss samples from the Shuanghe area in the Dabie Orogen, China. First, we analyzed only the zircon core or rim on each grain. Concordant ages of igneous zircon cores in two orthogneisses are 744 ? 10 and 768 ? 7 Ma, demonstrating that their protoliths were Neoproterozoic igneous rocks. The metamorphic zircon rims in the two granitic gneisses yielded a consistent weighted-mean 206Pb/238U age of 216 ? 2 Ma (2 SE; n = 12 and 17). Zircon grains in the studied eclogite are all metamorphic and yielded a weightedmean 206Pb/238U age of 224 ? 2 Ma (2 SE; n = 21). The different metamorphic ages of the eclogite and orthogneisses suggest that they might be juxtaposed by later tectonic events. After being repolished, zircon grains with apparent core?rim structures from the two granitic gneisses were re-analyzed in the cores and rims of each grain. Due to the small size of the zircon grains, the pre-sputtered areas of the two spots in each zircon overlapped. Compared with the analyses in the first session, the overlapping pre-sputtered areas affacted apparent dates for zircon rims by -8.2% to +13.2%. The age deviations of the second analyses correlate with the relative position of the overlaps. The apparent 206Pb/238U dates are younger when delta X 0 (i.e., the X coordinate of the second analysis is smaller than the first analysis), while the apparent 206Pb/238U dates are older when delta X 0. This study proves that erroneous SIMS U?Pb dates can be produced when dating metamorphic zircon rims after analyses of the cores with overlapping pre-sputtered areas. It will lead to an apparently longer and incorrect duration of a metamorphic event.
WOS关键词U-PB AGE ; ULTRAHIGH-PRESSURE ; DABIE MOUNTAINS ; ISOTOPE GEOCHEMISTRY ; O-18 DEPLETION ; EASTERN CHINA ; UHP ECLOGITES ; COUNTRY ROCKS ; SHUANGHE ; EVOLUTION
资助项目National Key Research and Development Program of China[2016YFE0203000] ; National Natural Science Foundation of China[41773044] ; National Natural Science Foundation of China[41673059] ; National Natural Science Foundation of China[41972059] ; National Program for Support of Top-Notch Young Professionals
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000647692100008
出版者ELSEVIER
资助机构National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals ; National Program for Support of Top-Notch Young Professionals
源URL[http://ir.iggcas.ac.cn/handle/132A11/101214]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Li, Qiuli
作者单位1.Hefei Univ Technol, Sch Resources & Environm Engn, Hefei 230029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Tang, Hu,Li, Qiuli,Liu, Yu,et al. Erroneous determination of the duration of metamorphism from analysis of overlapping pre-sputtered areas during SIMS U?Pb dating of zircon[J]. CHEMICAL GEOLOGY,2021,573:11.
APA Tang, Hu,Li, Qiuli,Liu, Yu,&Shi, Yonghong.(2021).Erroneous determination of the duration of metamorphism from analysis of overlapping pre-sputtered areas during SIMS U?Pb dating of zircon.CHEMICAL GEOLOGY,573,11.
MLA Tang, Hu,et al."Erroneous determination of the duration of metamorphism from analysis of overlapping pre-sputtered areas during SIMS U?Pb dating of zircon".CHEMICAL GEOLOGY 573(2021):11.

入库方式: OAI收割

来源:地质与地球物理研究所

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