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俯冲驱动地幔物质上涌与板内玄武岩质浆作用:以华南中生代HIMU型玄武岩为例
吴扬名; 郭锋; 章清文; 赵亮
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玄武岩 基性岩 地幔 地球内部 HIMU 板内 物质 华南
Abstract关于板内玄武岩的成因机制,前人提出了多种动力学模型,包括岩石圈伸展、加厚岩石圈拆沉、俯冲板片拆离等。这些动力学机制通常把板内玄武岩的源区局限在对流软流圈或岩石圈地幔。近年来随着认识程度的不断加深,具有洋岛玄武岩地球化学特征的岩浆很可能来自更深的地幔,如下地幔和地幔转换带。纵观全球中新世以来的小规模板内玄武
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35613
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
吴扬名,郭锋,章清文,等. 俯冲驱动地幔物质上涌与板内玄武岩质浆作用:以华南中生代HIMU型玄武岩为例[C],2017.
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