Oxidized conditions in iron meteorite parent bodies
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/s41561-018-0128-2.pdf
Reference43 articles.
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3. Brett, R. & Sato, M. Intrinsic oxygen fugacity measurements on 7 chondrites, a pallasite and a tektite and the redox state of the meteorite parent bodies. Geochim. Cosmochim. Acta 48, 111–120 (1984).
4. Cartier, C. et al. Experimental study of trace element partitioning between enstatite and melt in enstatite chondrites at low oxygen fugacities and 5 GPa. Geochim. Cosmochim. Acta 130, 167–187 (2014).
5. Bottke, W., Nesvorny, D., Grimm, R., Morbidelli, A. & O’Brien, D. Iron meteorites as remnants of planetesimals formed in the terrestrial planet region. Nature 439, 821–824 (2006).
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