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Australian Journal of Earth Sciences, Vol. 56, Iss. 7, 2009-10 ,pp. : 1003-1022

Taylor & Francis Ltd

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A subduction wedge origin for Paleoarchean peridotitic diamonds and harzburgites from the Panda kimberlite, Slave craton: evidence from Re–Os isotope systematics

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New method for separation of magnetite from rock samples for oxygen isotope analysis

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