Geochemical evolution of rocks at the base of the lithospheric mantle: Evidence from study of xenoliths of deformed peridotites from kimberlite of the Udachnaya pipe

被引：17
作者：
Agashev, A. M. [1 ,2 ]
Pokhilenko, N. P. [1 ]
Cherepanova, Yu. V. [1 ,3 ]
Golovin, A. V. [1 ]
机构：
[1] Russian Acad Sci, Siberian Branch, Sobolev Inst Geol & Mineral, Novosibirsk, Russia
[2] Univ St Etienne, St Etienne, France
[3] Univ Copenhagen, DK-1168 Copenhagen, Denmark
来源：
DOKLADY EARTH SCIENCES | 2010年 / 432卷 / 02期
基金：
俄罗斯基础研究基金会;
关键词：
SM-ND; CRATON; LHERZOLITES; SYSTEM; THICK;
D O I：
10.1134/S1028334X10060073
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
引用
收藏
页码：746 / 749
页数：4
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