Partitioning of MgO, FeO, NiO, MnO and Cr2O3 between magnesian silicate perovskite and magnesiowüstite: implications for the origin of inclusions in diamond and the composition of the lower mantle-Reference-Cited by-同舟云学术

Partitioning of MgO, FeO, NiO, MnO and Cr2O3 between magnesian silicate perovskite and magnesiowüstite: implications for the origin of inclusions in diamond and the composition of the lower mantle

Published:1992-07 Issue:2-4 Volume:111 Page:229-240
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Kesson S.E.,Fitz Gerald J.D.

Publisher

Elsevier BV

Subject

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

Reference31 articles.

1. The recognition of diamond inclusions, Part 1, Syngenetic mineral inclusions;Harris;Ind. Diamond Rev.,1968

2. Inclusions in diamond;Meyer,1987

3. Deep-Seated Inclusions in Kimberlites and the Problem of the Composition of the Upper Mantle;Sobolev,1977

4. Diamonds;Gurney,1989

5. Evidence for a 150–200 km thick Archaean lithosphere from diamond inclusion thermobarometry;Boyd;Nature,1985

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