Primary melting sequence of a deep (>250 km) lithospheric mantle as recorded in the geochemistry of kimberlite–carbonatite assemblages, Snap Lake dyke system, Canada-Reference-Cited by-同舟云学术

Primary melting sequence of a deep (>250 km) lithospheric mantle as recorded in the geochemistry of kimberlite–carbonatite assemblages, Snap Lake dyke system, Canada

Published:2008-10 Issue:3-4 Volume:255 Page:317-328
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Agashev A.M.,Pokhilenko N.P.,Takazawa E.,McDonald J.A.,Vavilov M.A.,Watanabe T.,Sobolev N.V.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference65 articles.

1. Sr and Nd isotope and geochemical features of Siberian Platform kimberlites;Agashev;Geologiya I Geofizika,2000

2. Geochemistry of Nakyn field kimberlites Siberia: evidence for an unique source composition;Agashev;Geology,2001

3. Rb–Sr and Sm–Nd isotopes in garnet-pyroxenite xenoliths from Siberian kimberlites: an insight into lithospheric mantle;Agashev;Journal of Mineralogical and Petrological Sciences,2001

4. Geochemistry and mineralogy of kimberlites from the Arkhangelsk region, NW Russia: evidence for transitional magma types;Beard;Lithos,2000

5. Systematics and energetics of trace-element partitioning between olivine and silicate melts: implications for the nature of mineral/melt partitioning;Beattie;Chemical Geology,1994

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