中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The effect of bulk rock composition in phase equilibria modelling: a case study of mafic granulites from the North China Craton

文献类型:期刊论文

作者Zou, Lei1,2,3,4; Guo, Jing-Hui1,2,4; Huang, Guang-Yu2,4; Jiao, Shu-Juan2,4; Tian, Zhong-Hua3; Liu, Ping-Hua3
刊名CONTRIBUTIONS TO MINERALOGY AND PETROLOGY
出版日期2022-02-01
卷号177期号:2页码:24
关键词Mafic granulite Phase equilibrium modelling Effective bulk composition Mismatch North China Craton
ISSN号0010-7999
DOI10.1007/s00410-022-01887-9
英文摘要A mafic granulite with relatively simple mineralogy and texture from the Miyun Complex in the northern part of the North China Craton is used to discuss the effect of bulk composition uncertainty determined by different techniques [X-ray fluorescence (XRF), mapping, and point counting] on the calculated phase diagrams. LA-ICP-MS U-Pb dating of zircon from this mafic granulite yields magmatic ages of similar to 2.5-2.45 Ga and metamorphic overprinting ages of similar to 1.8 Ga, consistent with previous results. Based on phase equilibrium modelling, we show that the topological relations of the P-T pseudo-sections calculated from the XRF and point-counting compositions are similar except for the K-feldspar and Fe-Ti oxide stability fields and that the mineral stability fields in the P-T pseudo-section calculated from the mapping composition are distinctly different from the others. Furthermore, the observed and calculated mineral compositions (X All in plagioclase) and mineral proportions (garnet and plagioclase) are matched in the P-T pseudo-section calculated from the point-counting composition, but these are mismatched in the P-T pseudo-section calculated from the mapping composition. For the P-T pseudo-section calculated from the XRF composition, mineral composition isopleths can further constrain the narrow P-T conditions but the observed and calculated mineral proportions do not match. Moreover, we obtain similar T conditions using geo-thermometers (Ti-in-amphibole, two-feldspar, and REE-in-Grt-Cpx geo-thermometers). In addition, we calculated the uncertainties (of the phase-in/out lines and the mineral-proportions and -compositions isopleths) on the thermodynamic modelling and discussed the main source of uncertainties in detail.
WOS关键词TEMPERATURE METAMORPHIC ROCKS ; P-T CONDITIONS ; MINERAL EQUILIBRIA ; HF ISOTOPES ; TRACE-ELEMENTS ; U-PB ; REACTION TEXTURES ; REACTION PROGRESS ; RARE-EARTH ; CONSTRAINTS
资助项目National Natural Science Foundation of China[41972205] ; National Natural Science Foundation of China[41890832] ; National Natural Science Foundation of China[41672191] ; Geological Investigation Project of the China Geological Survey[DD20190003] ; Geological Investigation Project of the China Geological Survey[DD20190370]
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
WOS记录号WOS:000749201600001
出版者SPRINGER
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey ; Geological Investigation Project of the China Geological Survey
源URL[http://ir.iggcas.ac.cn/handle/132A11/104021]  
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Liu, Ping-Hua
作者单位1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
3.Chinese Acad Geol Sci, Inst Geol, 26 Baiwanzhuang Rd, Beijing 100037, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
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Zou, Lei,Guo, Jing-Hui,Huang, Guang-Yu,et al. The effect of bulk rock composition in phase equilibria modelling: a case study of mafic granulites from the North China Craton[J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY,2022,177(2):24.
APA Zou, Lei,Guo, Jing-Hui,Huang, Guang-Yu,Jiao, Shu-Juan,Tian, Zhong-Hua,&Liu, Ping-Hua.(2022).The effect of bulk rock composition in phase equilibria modelling: a case study of mafic granulites from the North China Craton.CONTRIBUTIONS TO MINERALOGY AND PETROLOGY,177(2),24.
MLA Zou, Lei,et al."The effect of bulk rock composition in phase equilibria modelling: a case study of mafic granulites from the North China Craton".CONTRIBUTIONS TO MINERALOGY AND PETROLOGY 177.2(2022):24.

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来源:地质与地球物理研究所

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