[an error occurred while processing this directive] 世界地质 2023, 42(4) 621-635 DOI:     ISSN: 1004-5589 CN: 22-1111/P

本期目录 | 下期目录 | 过刊浏览 | 高级检索                                                            [打印本页]   [关闭]
基础地质
扩展功能
本文信息
Supporting info
PDF(3845KB)
[HTML全文]
参考文献[PDF]
参考文献
服务与反馈
把本文推荐给朋友
加入我的书架
加入引用管理器
引用本文
Email Alert
文章反馈
浏览反馈信息
本文关键词相关文章
地幔柱
橄榄岩包体
西伯利亚岩克拉通
 
本文作者相关文章
程哲
孙晶
PubMed
Article by Cheng Z
Article by Sun J
地幔柱活动对克拉通岩石圈地幔的影响: 西伯利亚克拉通地幔橄榄岩包体Sr-Nd-Hf同位素制约 
 程哲, 孙晶 
中国石油大学 (北京) 地球科学学院, 北京 102249 
摘要: 利用单矿物溶液法分析了 Obnazhennaya 金伯利岩中橄榄岩包体单矿物的Sr-Nd-Hf同位素组成, 并且与 Udachnaya 金伯利岩中橄榄岩包体单矿物的Sr-Nd-Hf同位素组成进行了对比? 结果显示, Ob? nazhennaya 金伯利岩中橄榄岩包体单斜辉石具有亏损的 Sr 同位素组成和富集的 Nd? Hf 同位素组成? 橄榄岩包体石榴子石的Sr-Nd-Hf同位素组成表现出原始的特征, 没有受到交代作用的影响? 通过对 比 Udachnaya 和 Obnazhennaya 金伯利岩中地幔包体的特征和单斜辉石的二元混合模拟发现, Udachnaya 金伯利岩中的地幔包体的 Sr ??Nd ??Hf 同位素组成更偏向于金伯利岩的特征, 而与之相反, Obnazhen? naya 金伯利岩中的地幔包体的Sr-Nd-Hf同位素组成则位于金伯利岩和地幔柱溢流玄武岩之间, 且更 加偏向于溢流玄武岩的同位素特征? 因此, 地幔柱活动对西伯利亚克拉通岩石圈产生了影响, 改变了 其岩石圈地幔的同位素组成?
关键词
Sr-Nd-Hf同位素   地幔柱   橄榄岩包体   西伯利亚岩克拉通
 
  
Effect of mantle plume activity on craton lithospheric mantle:Sr-Nd-Hfisotopic constraints of mantle peridotite xenoliths of Siberian Craton 
 CHENG Zhe, SUN Jing
College of Geosciences, China University of Petroleum, Beijing 102249, China 
Abstract: TheSr-Nd-Hfisotopic compositions of minerals in peridotite xenoliths from the Obnazhennaya kimberlite are analyzed using solution method, and compared with those from Udachnaya kimberlite. The results show that the clinopyroxenes within peridotite xenolith in the Obnazhennaya kimberlite are depleted in Sr and en? riched in Nd, Hf isotopic compositions. TheSr-Nd-Hfisotopic compositions of garnets from peridotite xenoliths in the Obnazhennaya kimberlite show primitive characteristics and are not affected by metasomatism. By comparing the characteristics of mantle xenoliths in Udachnaya and Obnazhennaya kimberlites and simulating binary mixing of cli? nopyroxenes, it is found that theSr-Nd-Hfisotopic composition of mantle xenoliths in Udachnaya kimberlite is quite similar to the characteristics of the hosting kimberlite, while theSr-Nd-Hfisotopic composition of mantle xen? oliths in Obnazhennaya kimberlite is of the character between kimberlite and basalt related to mantle plume, which is more close to the isotopic characteristics of basalt lava flow. Therefore, the mantle plume activity has an impact on the Siberian Craton lithosphere, changing the isotopic composition of its lithospheric mantle. 
Keywords: Sr-Nd-Hfisotopes   mantle plume   peridotite xenoliths   Siberian Craton  
收稿日期  修回日期  网络版发布日期  
DOI:
基金项目:

 

通讯作者:
作者简介:
作者Email:

参考文献:
 
本刊中的类似文章
1.刘金霖, 王建, 宋樾, 刘建国, 李爱.内蒙古阿尔山—柴河地区陆下岩石圈地幔性质研究 —第四纪碱性玄武岩中橄榄岩捕掳体中单斜辉石微量元素证据[J]. 世界地质, 2014,33(1): 1-10

Copyright by 世界地质