GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室  > 会议论文
为何月海玄武岩富铁
张明明; 朱丹; 许英奎; 章清文
Source Publication中国矿物岩石地球化学学会第九次全国会员代表大会暨第16届学术年会文集
2017-04-18
Conference Date2017-04-18
Conference Place中国陕西西安
Country中国
Indexed By其他
Language中文
Keyword岩浆洋 富铁 洋中脊玄武岩 地幔 地球内部 月球结构 月幔 月样 月海玄武岩
Abstract来自月海玄武岩和洋中脊玄武岩的样品表明,月海玄武岩FeO含量普遍高于洋中脊玄武岩。这意味着月幔相对于地幔更加富铁,这与多数学者获得的月岩浆洋成分一致(Sakai et al.,2014)。月震数据显示月核质量不超过月球总质量6%(Hood,1986),大碰撞模拟也显示撞击体核和地核对月球形成没有贡献(Canup,2004),因此月球的总铁含量
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35624
Collection中国科学院矿物学与成矿学重点实验室_会议论文
Recommended Citation
GB/T 7714
张明明,朱丹,许英奎,等. 为何月海玄武岩富铁[C],2017.
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