Geochemistry of 1.78Ga A-type granites along the southern margin of the North China Craton: implications for Xiong'er magmatism during the break-up of the supercontinent Columbia
Cui, Minli1,2; Zhang, Lianchang1; Zhang, Baolin1; Zhu, Mingtian1
刊名INTERNATIONAL GEOLOGY REVIEW
2013-03-01
卷号55期号:4页码:496-509
关键词North China Craton Palaeoproterozoic SIMS zircon UPb ages geochemistry A-type granite extension environment
ISSN号0020-6814
DOI10.1080/00206814.2012.736709
文献子类Article
英文摘要The Palaeoproterozoic Luoling granites occur along the southern margin of the North China Craton. They are rich in silica and total alkalis with SiO2 contents ranging from 65.18 to 72.72 wt.%, K2O from 4.68 to 6.62 wt.%, and Na2O from 1.35 to 4.88 wt.%. They have high Fe*[FeOt/(FeOt+ MgO)] ranging from 0.84 to 0.95 wt.% and low MnO (0.030.09 wt.%), MgO (0.271.55 wt.%), CaO (0.362.04 wt.%), TiO2 (0.41.12 wt.%), and P2O5 (0.040.36 wt.%). Geochemically, they show typical characteristics of A-type granites, such as high contents of alkalis (i.e. high K2O+ Na2O, with K2O/Na2O> 1), Rb, Y, Nb, and REEs (except for Eu); high FeOt/MgO and Ga/Al ratios; and low CaO, Al2O3, and Sr contents. New secondary ion mass spectroscopy (SIMS) zircon UPb ages reveal that the Luoling granites were emplaced at 1786 +/- 7 Ma and thus were approximately coeval with Xiong'er volcanic rocks in the area. Their negative bulk-rock initial Nd and zircon initial Hf isotopic ratios suggest that they have affinities to EM-I-type mantle and both are the products of Xiong'er magmatism during the Palaeoproterozoic. We regard them as produced under a continental rift setting during the Palaeoproterozoic, genetically related to the break-up of the Columbia supercontinent.
WOS关键词ULTRAHIGH-TEMPERATURE METAMORPHISM ; TRACE-ELEMENT ; HF ISOTOPES ; LU-HF ; PALEOPROTEROZOIC EVOLUTION ; POSTCOLLISIONAL MAGMATISM ; TECTONIC EVOLUTION ; PETROGENESIS ; ZIRCON ; PB
WOS研究方向Geology
语种英语
出版者TAYLOR & FRANCIS INC
WOS记录号WOS:000314348400007
资助机构Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; Chinese Academy of Sciences(KZCX2-YW-Q04-07) ; Chinese Academy of Sciences(KZCX2-YW-Q04-07) ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; Chinese Academy of Sciences(KZCX2-YW-Q04-07) ; Chinese Academy of Sciences(KZCX2-YW-Q04-07) ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; Chinese Academy of Sciences(KZCX2-YW-Q04-07) ; Chinese Academy of Sciences(KZCX2-YW-Q04-07) ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; Chinese Academy of Sciences(KZCX2-YW-Q04-07) ; Chinese Academy of Sciences(KZCX2-YW-Q04-07)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/87085]  
专题中国科学院地质与地球物理研究所
通讯作者Zhang, Lianchang
作者单位1.Chinese Acad Sci, Key Lab Mineral Resources, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Dev Res Ctr China Geol Survey, Beijing 100037, Peoples R China
推荐引用方式
GB/T 7714
Cui, Minli,Zhang, Lianchang,Zhang, Baolin,et al. Geochemistry of 1.78Ga A-type granites along the southern margin of the North China Craton: implications for Xiong'er magmatism during the break-up of the supercontinent Columbia[J]. INTERNATIONAL GEOLOGY REVIEW,2013,55(4):496-509.
APA Cui, Minli,Zhang, Lianchang,Zhang, Baolin,&Zhu, Mingtian.(2013).Geochemistry of 1.78Ga A-type granites along the southern margin of the North China Craton: implications for Xiong'er magmatism during the break-up of the supercontinent Columbia.INTERNATIONAL GEOLOGY REVIEW,55(4),496-509.
MLA Cui, Minli,et al."Geochemistry of 1.78Ga A-type granites along the southern margin of the North China Craton: implications for Xiong'er magmatism during the break-up of the supercontinent Columbia".INTERNATIONAL GEOLOGY REVIEW 55.4(2013):496-509.
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