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Repeated recharge of primitive melts in the lower oceanic crust: Constraints from the Dongco ophiolite, Central Tibet
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DOI：10.1016/j.lithos.2026.108709.png)
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Abstract
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• Poikilitic textures and vermicular orthopyroxene indicate disequilibrium reactions. • Cr zoning in clinopyroxene reflects repeated injections of primitive melts. • Primitive melt recharge modified cumulate mineralogy and chemistry.
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