The limitations of hibonite as a single-mineral oxybarometer for early solar system processes-Reference-Cited by-同舟云学术

The limitations of hibonite as a single-mineral oxybarometer for early solar system processes

Published:2017-09 Issue: Volume:466 Page:32-40
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Berry Andrew J.,Schofield Paul F.,Kravtsova Antonina N.,Miller Laura A.,Stephen Natasha R.,Walker Andrew M.,Soldatov Alexander V.,Ireland Trevor R.,Geraki K.,Mosselmans J. Fred W.

Funder

Australian Research Council

Ministry of Education and Science of the Russian Federation

Natural Environment Research Council for an Independent Research Fellowship

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference32 articles.

1. The stability of hibonite, melilite and other aluminous phases in silicate melts: implications for the origin of hibonite-bearing inclusions from carbonaceous chondrites;Beckett;Meteoritics,1994

2. Ti3+ in meteoritic and synthetic hibonite;Beckett;Geochim. Cosmochim. Acta,1988

3. A XANES determination of the oxidation state of chromium in silicate glasses;Berry;Am. Mineral.,2004

4. Titanium substitution mechanisms in forsterite;Berry;Chem. Geol.,2007

5. The oxidation state of iron in komatiitic melt inclusions indicates hot Archaean mantle;Berry;Nature,2008

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