Chromium isotope fractionation during subduction-related metamorphism, black shale weathering, and hydrothermal alteration
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文摘

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

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