Magnesium isotopic homogeneity of San Carlos olivine: a potential standard for Mg isotopic analysis by multi-collector inductively coupled plasma mass spectrometry
Previous analyses on San Carlos olivine from Arizona (USA) have shown inter-laboratory δ26Mg differences of up to 0.67‰, while mantle olivine samples worldwide are homogeneous at a current analytical uncertainty of ~0.1‰. The differing measurements on San Carlos olivine may be attributable to analytical artifacts or sample heterogeneity. The latter must be ruled out before using it as a standard for Mg isotopic analysis.