Undetectable δ53Cr variation in high temperature rocks
Undetectable δ53Cr variation in a metacarbonate transect that is representative of fluid-rich regional metamorphism
Up to 1‰ δ53Cr variation in a low pH black shale weathering profile
Undetectable δ53Cr variation in mildly altered upper oceanic crust
High δ53Cr and low [Cr] in serpentinized peridotites