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

页码：746 / 749

页数：4

共 15 条

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