Geochemistry and tectonic implications of rhyolites from Yingcheng Formation in Xujiaweizi, Songliao Basin. | |
Meng FanChao1; Liu JiaQi1; Li Ming2; Liu Xiao2; Yin ChangHai3; Lu JiaMin3; Cui Yan4 | |
刊名 | ACTA PETROLOGICA SINICA |
2010 | |
卷号 | 26期号:1页码:227-241 |
关键词 | Songliao Basin Yingcheng Formation Rhyolite Geochemistry Tectonic significance |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | The intermediate-felsic rocks, mainly rhyolites, are widely distributed in Yingcheng Formation in Xujiaweizi, Songliao Basin. Petrological, major and trace elements geochemistry Studies exhibit that the content of many elements (e.g. Si, K, Rb) of the rhyolites is a little influenced by burial and regional metamorphism, low-temperature hydration and hydrothermal alteration. The rhyolites are prominently enriched strongly incompatible elements Such as Rb, Th, U, Pb, and have apparently negative Ba, Sr, Ti, Eu, P anomalies, which indicate the rocks were produced by fractional crystallization of plagioclase, apatite and ilmenite. The rhyolites have high and wide initial (87)Sr/(86)Sr (0.705265 similar to 711895) ratios. Most epsilon(ND) (t) values of the rhyolites are all positive and have a narrow range (1.83 similar to 3.38), but they have an analogical radiogenic Pb (((206)Pb/(204)Pb)(i) = 18.09 similar to 18.32, ((207)pb/(204)Pb)(i) = 15.50 similar to 15.54, ((208)Pb/(204)Pb)(i) = 37.80 similar to 38.10). The features of isotopic data indicate that the primary, magmas were derived originated from a mixed source by juvenile component and ancient crust, but contaminated by the crust in different level during evolution. The rhyolites may erupt in extensional setting within plate in the Early Cretaceous, and were probably associated with the lithospheric thinning and asthenospheric mantle upwelling by subduction of the Pacific plate beneath eastern China. |
WOS关键词 | A-TYPE GRANITES ; DA-HINGGAN MOUNTAINS ; PHANEROZOIC CRUSTAL GROWTH ; FELSIC VOLCANIC-ROCKS ; GREAT XINGAN RANGE ; NE CHINA ; NORTHEASTERN CHINA ; CHEMICAL CLASSIFICATION ; ISOTOPIC CONSTRAINTS ; MAGMATIC EVOLUTION |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000274509500025 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/72214] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Meng FanChao |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China 3.Daqing Oil Field, Res Inst Petr Explorat & Dev, Daqing 163712, Peoples R China 4.Shengli Oil Field, Res Inst Geol Sci, Dongying 257015, Peoples R China |
推荐引用方式 GB/T 7714 | Meng FanChao,Liu JiaQi,Li Ming,et al. Geochemistry and tectonic implications of rhyolites from Yingcheng Formation in Xujiaweizi, Songliao Basin.[J]. ACTA PETROLOGICA SINICA,2010,26(1):227-241. |
APA | Meng FanChao.,Liu JiaQi.,Li Ming.,Liu Xiao.,Yin ChangHai.,...&Cui Yan.(2010).Geochemistry and tectonic implications of rhyolites from Yingcheng Formation in Xujiaweizi, Songliao Basin..ACTA PETROLOGICA SINICA,26(1),227-241. |
MLA | Meng FanChao,et al."Geochemistry and tectonic implications of rhyolites from Yingcheng Formation in Xujiaweizi, Songliao Basin.".ACTA PETROLOGICA SINICA 26.1(2010):227-241. |
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