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Subduction zone mantle enrichment by fluids and Zr-Hf-depleted crustal melts as indicated by backarc basalts of the Southern Volcanic Zone, Argentina
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文摘

Backarc mantle metasomatized by contrasting types of subducted upper continental crust

One type of mantle-enriching crustal melts had low Zr/Sm and Hf/Sm due to residual zircon.

Depleted and undepleted pre-metasomatic mantle mixed during Pleistocene slab steepening

Three types of mantle sourced Transitional Southern Volcanic Zone arc magmas

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