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Fluid-related modifications of Cr-spinel and olivine from ophiolitic peridotites by contact metamorphism of granitic intrusions in the Ablah area, Saudi Arabia
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The Ablah peridotites are partly or fully serpentinized due to contact metamorphism.

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Three distinct modification patterns of Cr-spinel are identified.

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Simple zoning with sharp contacts between cores and rims results from solid-state alteration.

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Weakly zoned and atoll-textured patterns result from high fluid/rock ratio alteration.

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Petrogenesis and metamorphic evolution of Ablah peridotites are predicted.

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