CORC  > 国家天文台  > 中国科学院国家天文台  > 院士
Mineralogical variation of the late stage mare basalts
Zhang, Xunyu1; Wu, Yunzhao2; Ouyang, Ziyuan3; Bugiolacchi, Roberto1; Chen, Yuan2; Zhang, Xiaomeng2,4; Cai, Wei2; Xu, Aoao1; Tang, Zesheng1
刊名JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
2016-10-01
卷号121期号:10页码:2063-2080
关键词late stage mare basalt mineralogical variations mapping spectral analysis high-Ti basalt
英文摘要The last major phases of lunar volcanism occurred mainly in Oceanus Procellarum and Mare Imbrium and produced spectrally unique medium- and high-titanium basalts. The composition and distribution of these basalts provide a record of the late stage thermal evolution of the Moon. To study the spectral and mineralogical variations of the late stage mare basalts, 31 distinct units were mapped employing a range of remote sensing data. Their inferred mineralogical characteristics were studied by analyzing the spectral features of small, fresh craters derived from the Moon Mineralogy Mapper (M-3) data. The strongest olivine spectral signatures were found around Lichtenberg crater, while the units with the lowest olivine/pyroxene ratio occurred mainly in the southern Kepler crater and some local areas. In Oceanus Procellarum, the olivine/pyroxene ratio decreases progressively from the Lichtenberg crater to the southern units. The northern and southern units within Mare Imbrium have higher olivine/pyroxene ratios than the central ones. The inferred abundance of olivine appears to vary stratigraphically, with the younger flows being more olivine rich. However, the stratigraphically younger units around Euler crater in Mare Imbrium, which present as dark red hues in the integrated band depth image of M-3, were found to have lower olivine/pyroxene ratios than the units around Lichtenberg crater (shown as light red hues) in Oceanus Procellarum. It could be interpreted that the late stage mare basalts around Lichtenberg crater originated from a more olivine-rich source than those around Euler crater.
WOS标题词Science & Technology ; Physical Sciences
类目[WOS]Geochemistry & Geophysics
研究领域[WOS]Geochemistry & Geophysics
关键词[WOS]PROCELLARUM KREEP TERRANE ; OCEANUS PROCELLARUM ; REFLECTANCE SPECTROSCOPY ; SPECTRAL REFLECTANCE ; PYROXENE MIXTURES ; LUNAR BASALTS ; CLEMENTINE ; VOLCANISM ; MOON ; IRON
收录类别SCI
语种英语
WOS记录号WOS:000387795800012
内容类型期刊论文
源URL[http://ir.bao.ac.cn/handle/114a11/6853]  
专题国家天文台_院士
作者单位1.Macau Univ Sci & Technol, Space Sci Inst, Macau, Peoples R China
2.Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing, Jiangsu, Peoples R China
3.Chinese Acad Sci, Natl Astron Observ, Beijing, Peoples R China
4.Jiangsu Ctr Collaborat Innovat Geog Informat Res, Nanjing, Jiangsu, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Xunyu,Wu, Yunzhao,Ouyang, Ziyuan,et al. Mineralogical variation of the late stage mare basalts[J]. JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS,2016,121(10):2063-2080.
APA Zhang, Xunyu.,Wu, Yunzhao.,Ouyang, Ziyuan.,Bugiolacchi, Roberto.,Chen, Yuan.,...&Tang, Zesheng.(2016).Mineralogical variation of the late stage mare basalts.JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS,121(10),2063-2080.
MLA Zhang, Xunyu,et al."Mineralogical variation of the late stage mare basalts".JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS 121.10(2016):2063-2080.
个性服务
查看访问统计
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。


©版权所有 ©2017 CSpace - Powered by CSpace