globalchange  > 气候减缓与适应
DOI: 10.1002/grl.50966
论文题名:
NAL phase in K-rich portions of the lower mantle
作者: Kato C.; Hirose K.; Komabayashi T.; Ozawa H.; Ohishi Y.
刊名: Geophysical Research Letters
ISSN: 0094-8511
EISSN: 1944-8242
出版年: 2013
卷: 40, 期:19
起始页码: 5085
结束页码: 5088
语种: 英语
英文关键词: Al phase ; CF phase ; high pressure ; lower mantle ; NAL phase ; phase relation
Scopus关键词: Al phase ; High pressure ; Lower mantle ; NAL phase ; Phase relation ; High pressure engineering ; Potassium ; Silicon ; Structural geology ; X ray diffraction ; Aluminum ; aluminum ; core-mantle boundary ; diamond anvil cell ; heat source ; high pressure ; low velocity zone ; lower mantle ; magma chamber ; partial melting ; potassium ; seismology ; X-ray diffraction
英文摘要: The stability of the K-rich new aluminous (NAL) phase was examined on the join Na1.00Mg2.00Al4.80Si1.15O 12-K1.00Mg2.00Al4.80Si 1.15O12 (Na100-K100) up to 144 GPa by X-ray diffraction in a laser-heated diamond anvil cell. Single-phase K100 and Na50K50 NAL were formed up to the lower mantle conditions, and the NAL phase coexisted with the calcium ferrite-type (CF) phase at 120 GPa and 2300 K for the Na75K25 bulk composition. This is a striking contrast to the K-free (Na100) NAL that becomes unstable above 27 GPa at 1850 K, which suggests that potassium stabilizes NAL at significantly higher pressures. K-rich NAL may host potassium in the lower mantle that contains K2O more than 0.09 wt %. In addition, the NAL phase likely formed owing to partial melting in the ultralow-velocity zone or because of a basal magma ocean. Future seismological observations may clarify whether NAL is a radiogenic heat source above the core-mantle boundary. Key Points Potassium expands the stability of the NAL phase dramatically K-rich NAL is stable o the lowermost mantle conditions NAL forms in the whole lower mantle where the K2O content is higher than 900 ppm ©2013. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84884998125&doi=10.1002%2fgrl.50966&partnerID=40&md5=60b65a1f65f71f2a7d873b913ddb4067
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/5775
Appears in Collections:气候减缓与适应

Files in This Item:

There are no files associated with this item.


作者单位: Department of Earth and Planetary Sciences, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro, Tokyo 152-8551, Japan

Recommended Citation:
Kato C.,Hirose K.,Komabayashi T.,et al. NAL phase in K-rich portions of the lower mantle[J]. Geophysical Research Letters,2013-01-01,40(19).
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Kato C.]'s Articles
[Hirose K.]'s Articles
[Komabayashi T.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Kato C.]'s Articles
[Hirose K.]'s Articles
[Komabayashi T.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Kato C.]‘s Articles
[Hirose K.]‘s Articles
[Komabayashi T.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.