Honda, MasahikoPhillips, DavidKendrick, MarkGagan, MichaelTaylor, W.R.2015-12-100812-0099http://hdl.handle.net/1885/69552The Argyle lamproite pipe of Western Australia contains diamonds formed at depths exceeding 150 km. We undertook noble gas and carbon isotope ratio (δ13C) analyses of three diamonds (likely of eclogitic paragenesis) from the Argyle lamproite to test forKeywords: argon isotope; carbon isotope ratio; continental lithosphere; diamond; helium; isotopic composition; lamproite; mantle structure; noble gas; subduction; xenon; Australia; Western Australia carbon; continental lithosphere; diamond; mantle evolution; noble gas; subductionNoble gas and carbon isotope ratios in Argyle diamonds, Western Australia: Evidence for a deeply subducted volatile component201210.1080/08120099.2012.7410762016-02-24