Timing of lunar Mg-suite magmatism constrained by SIMS U-Pb dating of Apollo norite 78238
文献类型:期刊论文
作者 | Zhang, Bidong3,4; Lin, Yangting2; Moser, Desmond E.4; Warren, Paul H.3; Hao, Jialong2; Barker, Ivan R.4; Shieh, Sean R.4; Bouvier, Audrey1,4 |
刊名 | EARTH AND PLANETARY SCIENCE LETTERS
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出版日期 | 2021-09-01 |
卷号 | 569页码:10 |
关键词 | U-Pb Mg-suite SIMS baddeleyite zircon lunar magma ocean |
ISSN号 | 0012-821X |
DOI | 10.1016/j.epsl.2021.117046 |
英文摘要 | The lunar Mg-suite magmatic rocks are commonly thought to represent mafic intrusions into the anorthositic flotation crust of the lunar magma ocean (LMO). Their geochronology is, therefore, important for constraining evolution models of the LMO. Petrogenetic models of the Mg-suite hold that their parent magmas were derived from primary LMO sources (Mg-cumulates, An-rich plagioclase, and melts enriched in KREEP-potassium, rare earth elements, and phosphorus). Previous radiogenic isotopic age interpretations of Mg-suite and putatively older, related ferroan anorthosites (FANs) overlap over a 200-million-year interval. The Apollo 78238 norite is an exemplary Mg-suite rock, with a relict coarse igneous texture modified by shock metamorphism. In-situsecondary ion mass spectrometry U-Pb analyses of zircon and baddeleyite in 78238 yield discordant arrays, attributed to recent impact metamorphism, with upper intercepts that constrain its crystallization age. The four oldest baddeleyite analyses give a weighted mean Pb-207/Pb-206 age of 4332 +/- 18 Ma (2s, MSWD = 0.06, P = 0.98), which is interpreted as the crystallization age of the norite. The overlap of the baddeleyite age with previously reported Sm-Nd and Pb-Pb mineral isochron ages for 78238 (Edmunson et al., 2009) supports a moderately fast cooling of the norite. Moreover, it is distinguishably younger than the most precisely dated sample of FAN (Apollo 60025), measured at 4360 +/- 3 Ma by Sm-Nd and Pb-Pb mineral isochrons (Borg et al., 2011). Together with the baddeleyite Pb-207/Pb-206 age of Apollo Mg-suite troctolite 76535 at 4328 +/- 8 Ma (White et al., 2020), the chronological record of the 78238 norite indicates a significant Mg-suite magmatic event at 4.33 Ga and a lower age limit on LMO differentiation. (C) 2021 The Author(s). Published by Elsevier B.V. |
WOS关键词 | EARTH ; DIFFUSION ; CRUST ; MOON ; CRYSTALLIZATION ; TEMPERATURE ; SYSTEMATICS ; EVOLUTION ; PETROLOGY ; HISTORY |
资助项目 | Canada Research Chairs[950-229061] ; NSERC[06818-2019] ; NSERC[06310-2014] ; NSERC[2019-05911] ; Natural Science Foundation of China[41490631] ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences[QYZDJ-SSW-DQC001] ; China Scholarship Council[201607970013] ; NASA[80NSSC19K1238] ; NASA[80NSSC19K0794] |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
WOS记录号 | WOS:000671231800002 |
出版者 | ELSEVIER |
资助机构 | Canada Research Chairs ; Canada Research Chairs ; NSERC ; NSERC ; Natural Science Foundation of China ; Natural Science Foundation of China ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; NASA ; NASA ; Canada Research Chairs ; Canada Research Chairs ; NSERC ; NSERC ; Natural Science Foundation of China ; Natural Science Foundation of China ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; NASA ; NASA ; Canada Research Chairs ; Canada Research Chairs ; NSERC ; NSERC ; Natural Science Foundation of China ; Natural Science Foundation of China ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; NASA ; NASA ; Canada Research Chairs ; Canada Research Chairs ; NSERC ; NSERC ; Natural Science Foundation of China ; Natural Science Foundation of China ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, Chinese Academy of Sciences ; China Scholarship Council ; China Scholarship Council ; NASA ; NASA |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/101991] ![]() |
专题 | 地质与地球物理研究所_中国科学院地球与行星物理重点实验室 |
通讯作者 | Zhang, Bidong |
作者单位 | 1.Univ Bayreuth, Bayer Geoinst, D-95447 Bayreuth, Germany 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China 3.Univ Calif Los Angeles, Dept Earth Planetary & Space Sci, Los Angeles, CA 90095 USA 4.Univ Western Ontario, Dept Earth Sci, London, ON N6A 3K7, Canada |
推荐引用方式 GB/T 7714 | Zhang, Bidong,Lin, Yangting,Moser, Desmond E.,et al. Timing of lunar Mg-suite magmatism constrained by SIMS U-Pb dating of Apollo norite 78238[J]. EARTH AND PLANETARY SCIENCE LETTERS,2021,569:10. |
APA | Zhang, Bidong.,Lin, Yangting.,Moser, Desmond E..,Warren, Paul H..,Hao, Jialong.,...&Bouvier, Audrey.(2021).Timing of lunar Mg-suite magmatism constrained by SIMS U-Pb dating of Apollo norite 78238.EARTH AND PLANETARY SCIENCE LETTERS,569,10. |
MLA | Zhang, Bidong,et al."Timing of lunar Mg-suite magmatism constrained by SIMS U-Pb dating of Apollo norite 78238".EARTH AND PLANETARY SCIENCE LETTERS 569(2021):10. |
入库方式: OAI收割
来源:地质与地球物理研究所
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