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Greenwood, R.C.; Franchi, I.A. and Jambon, A.
(2006).
URL: http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1768...
Abstract
High precision oxygen isotope analyses reveal that the silicate portion of mesosiderites are indistinguishable from the HEDs and suggest a common origin. However, the main group pallasites have a distinct signature, and therefore different source.
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- Item ORO ID
- 8463
- Item Type
- Conference or Workshop Item
- Extra Information
- Abstract #1768
- Academic Unit or School
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Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Depositing User
- Kyra Proctor