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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.