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4. Parent Bodies of Iron Meteorites

Published online by Cambridge University Press:  12 April 2016

Abstract

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On the basis of their chemical and mineralogical composition, 420 iron meteorites have been classified into 12 different groups. Each group seems to have come from a separate parent body. The largest group, IIIAB, probably formed an asteroidal core in a body approximately 100 km in radius, which was largely destroyed by collision 630 My ago. Another 67 analyzed irons do not belong to these groups, and may represent samples from another 20 or more bodies.

Type
Part VII. Differentiated Meteorites
Copyright
Copyright © A.H. Delsemme 1977

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