Os–Hf–Sr–Nd isotope and PGE systematics of spinel peridotite xenoliths from Tok, SE Siberian craton: Effects of pervasive metasomatism in shallow refractory mantle

Author:

Ionov Dmitri A.,Shirey Steven B.,Weis Dominique,Brügmann Gerhard

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference74 articles.

1. Mantle samples included in volcanic rocks: xenoliths and diamonds;Pearson,2003

2. Re–Os, Sm–Nd, and Rb–Sr isotope evidence for thick Archaean lithospheric mantle beneath the Siberian craton modified by multistage metasomatism;Pearson;Geochim. Cosmochim. Acta,1995

3. Radiogenic isotopes and REE in garnet peridotite xenoliths from the Mir kimberlite pipe, Yakutia;Zhuravlev;Geochem. Int.,1992

4. Lithospheric mantle beneath the south-eastern Siberian craton: petrology of peridotite xenoliths in basalts from the Tokinsky Stanovik;Ionov;Contrib. Mineral. Petrol.,2005

5. Origin of Fe-rich lherzolites and wehrlites from Tok, SE Siberia by reactive melt percolation in refractory mantle peridotites;Ionov;Contrib. Mineral. Petrol.,2005

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