The high-pressure structure of kaersutite and its geological importance. | |
Zhu, XP; Qin, S; Han, BF; Liu, J; Li, XD; Wu, X; Wu, ZH; Liu J(刘景); Li XD(李晓东); Wu X(巫翔) | |
刊名 | ACTA PETROLOGICA SINICA |
2004 | |
卷号 | 20期号:6页码:1456-1460 |
关键词 | kaersutite high-pressure structure synchrotron radiation |
通讯作者 | Peking Univ, Dept Geol, MOE, Beijing 100871, Peoples R China ; Peking Univ, Key Lab Orogen Belts & Crustal Evolut, MOE, Beijing 100871, Peoples R China ; Chinese Acad Sci, Inst High Energy Phys, Lab Synchrotron Radiat, Beijing 100039, Peoples R China |
英文摘要 | The in-situ high-pressure structure of natural kaersutite, obtained from the mantle xenolith in alkali basalt of southwestern Tianshan in Xinjiang, has been studied using synchrotron radiation energy dispersive X-ray diffraction and diamond anvil cell at the pressures up to 25.4 GPa. At room temperature, the lattice constants a, b, c of kaersutite are compressed continuously with increasing pressure and at the pressure of 18.9 GPa, a phase transition occurs probably due to the dehydration. Considering the geological occurrence of kaersutite, the experimental results indicate that kaersutite could be stable with rather a depth in the upper mantle, and it must be a rapid process when kaersutite is brought to the earth's surface. In addition, this research would be potentially helpful for the understanding of high-pressure behaviors of other Ti-bearing minerals. |
学科主题 | Geology |
类目[WOS] | Geology |
研究领域[WOS] | Geology |
原文出处 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000226179100015 |
内容类型 | 期刊论文 |
源URL | [http://ir.ihep.ac.cn/handle/311005/239361] |
专题 | 高能物理研究所_多学科研究中心 |
作者单位 | 中国科学院高能物理研究所 |
推荐引用方式 GB/T 7714 | Zhu, XP,Qin, S,Han, BF,et al. The high-pressure structure of kaersutite and its geological importance.[J]. ACTA PETROLOGICA SINICA,2004,20(6):1456-1460. |
APA | Zhu, XP.,Qin, S.,Han, BF.,Liu, J.,Li, XD.,...&吴忠华.(2004).The high-pressure structure of kaersutite and its geological importance..ACTA PETROLOGICA SINICA,20(6),1456-1460. |
MLA | Zhu, XP,et al."The high-pressure structure of kaersutite and its geological importance.".ACTA PETROLOGICA SINICA 20.6(2004):1456-1460. |
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