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Busemann, H.; Lorenzetti, S. and Eugster, O.
(2004).
URL: http://www.lpi.usra.edu/meetings/lpsc2004/pdf/1705...
Abstract
We compare the noble gases in D'Orbigny glass and bulk. The glass was formed after the bulk silicates and contains interior solar noble gases that may originate from early volcanic activity on the angrite parent body, trapped upon fast cooling.