Published September 2000 | Version Published
Journal Article Open

Rhenium-osmium fractionation in group IIIAB iron meteorites

Abstract

Group IIIAB is a large iron meteorite group, showing compositional trends suggestive of formation by extensive fractional crystallization of a magma. However, there are problerus in explaining some key IIIAB trends using simple fractional crystallization models and published partition coefficients.

Additional Information

© 2010 The Meteoritical Society.

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Identifiers

Eprint ID
47219
DOI
10.1111/j.1945-5100.2000.tb01796.x
Resolver ID
CaltechAUTHORS:20140715-101539223

Dates

Created
2014-07-15
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Updated
2021-11-10
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