中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geochemistry of Zhalantun dyke swarm in north Da Hinggan Mountain and its geological implication

文献类型:期刊论文

作者Zhang YuTao; Zhang LianChang; Ying JiFeng; Zhou XinHua
刊名ACTA PETROLOGICA SINICA
出版日期2006-11-01
卷号22期号:11页码:2733-2742
关键词Zhalantun dyke swarm petrogeochemistry remelting of the lower crust Da Hinggan Mountain
ISSN号1000-0569
文献子类Article
英文摘要Zhalantun dyke swarm was emplaced in a late Carboniferous Zhalantun granitic pluton, Inner Mongolia. The dyke swarm consists of diorite porphyrite in lithology. The samples all have porphyraceous texture. Phenocrysts are plagioclase,alkalic feldspar, hornblende,pyroxene and quartz, matrixes are fine-grained minerals above mentioned and glass. Zircon U-Pb determination yields a concordant age of 120.6 +/- 4.7 Ma and Ar-40-Ar-39 dating of the matrix gives a plateau age of 122.2 +/- 0.6Ma, indicating intrusive time of the dyke swarm is the early Cretaceous. The chemical analyses of the dyke swarm show that SiO, contents have a range of 56.88% similar to 61.69%, Al2O3 contents range from 15.83% to 19.29%, and total alkali is high (5.32% similar to 8.37%). The total REE contents have a large variation, ranging from 121.4 x 10(-6) to 144.1 X 10(-6). The samples have high ( La/Yb), Values (6.24 similar to 10.40) and little negative Eu anomaly ( 0.92 similar to 0.79). The samples are enriched in LILE and depleted in HFSE. Isotopic geochemistry shows that the dykes have high epsilon(Nd) ( t) of + 3.06 and low ( Sr-87/Sr-86)(i) of 0.7047 similar to 0.7053 and Pb characteristics similar to those of mantle. According to the geochemistry and geochronology of the dyke swarm and compared to the contemporary volcanic rocks, we concluded that the dykes originated from the remelting of the underplating basaltic juvenile lower crust.
WOS关键词I-TYPE GRANITES ; CRUSTAL GROWTH ; NORTHEASTERN CHINA ; NE CHINA ; ISOTOPIC CONSTRAINTS ; U-PB ; PETROGENESIS ; ORIGIN ; EXTENSION ; MONGOLIA
WOS研究方向Geology
语种英语
WOS记录号WOS:000242929100011
出版者SCIENCE CHINA PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/66758]  
专题中国科学院地质与地球物理研究所
通讯作者Zhang YuTao
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China
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Zhang YuTao,Zhang LianChang,Ying JiFeng,et al. Geochemistry of Zhalantun dyke swarm in north Da Hinggan Mountain and its geological implication[J]. ACTA PETROLOGICA SINICA,2006,22(11):2733-2742.
APA Zhang YuTao,Zhang LianChang,Ying JiFeng,&Zhou XinHua.(2006).Geochemistry of Zhalantun dyke swarm in north Da Hinggan Mountain and its geological implication.ACTA PETROLOGICA SINICA,22(11),2733-2742.
MLA Zhang YuTao,et al."Geochemistry of Zhalantun dyke swarm in north Da Hinggan Mountain and its geological implication".ACTA PETROLOGICA SINICA 22.11(2006):2733-2742.

入库方式: OAI收割

来源:地质与地球物理研究所

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