中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Cluster of water molecules in garnet of eclogite: an evidence of the existence of fluid during ultra-high pressure metamorphic process.

文献类型:期刊论文

作者Su, W; You, ZD; Zhong, ZQ; Chen, DZ; Guo, LH
刊名ACTA PETROLOGICA SINICA
出版日期2001-10-01
卷号17期号:4页码:643-647
关键词clusters of water molecules in garnet UHP metamorphic fluid Dabie Mountains
ISSN号1000-0569
文献子类Article
英文摘要Clusters of water molecules within garnet, which comes from foliated eclogite of ultra-high pressure metamorphic belt from the Dabie Mountains, is identified by transmission electron microscopy. This indicates that garnet, as a carrier of fluids, is able to bring water into the mantle while continental rocks were subducted. And clusters of water molecules within garnet are very important evidence of the existence of fluid during ultra-high pressure metamorphic process.
WOS关键词EAST-CENTRAL CHINA ; DABIE MOUNTAINS ; ISOTOPE ; COESITE ; PYROPE ; OXYGEN ; GEOCHEMISTRY ; SOLUBILITY ; COMPONENT ; HYDROXYL
WOS研究方向Geology
语种英语
WOS记录号WOS:000172356500015
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/76579]  
专题中国科学院地质与地球物理研究所
通讯作者Su, W
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Nanjing Univ, State Key Lab Mineral Deposits, Nanjing 210008, Peoples R China
3.China Univ Geosci, Wuhan 430074, Peoples R China
4.China Univ Geosci, Beijing 100083, Peoples R China
5.Chinese Acad Geol Sci, Inst Mineral Deposits, Beijing 100037, Peoples R China
推荐引用方式
GB/T 7714
Su, W,You, ZD,Zhong, ZQ,et al. Cluster of water molecules in garnet of eclogite: an evidence of the existence of fluid during ultra-high pressure metamorphic process.[J]. ACTA PETROLOGICA SINICA,2001,17(4):643-647.
APA Su, W,You, ZD,Zhong, ZQ,Chen, DZ,&Guo, LH.(2001).Cluster of water molecules in garnet of eclogite: an evidence of the existence of fluid during ultra-high pressure metamorphic process..ACTA PETROLOGICA SINICA,17(4),643-647.
MLA Su, W,et al."Cluster of water molecules in garnet of eclogite: an evidence of the existence of fluid during ultra-high pressure metamorphic process.".ACTA PETROLOGICA SINICA 17.4(2001):643-647.

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来源:地质与地球物理研究所

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