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Subduction-related metasomatic mantle source in the eastern Central Asian Orogenic Belt: Evidence from amphibolites in the Xilingol Complex, Inner Mongolia, China
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文摘
Mafic rocks in northern accretionary zone of CAOB record 340–309 Ma extension. The rocks derived from a depleted mantle source but enriched by oceanic slab. Mantle-derived magma and oceanic crust recycling affected the primitive magma.

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