Multiple origins for the Middle Jurassic to Early Cretaceous high-K calc-alkaline I-type granites in northwestern Fujian province, SE China and tectonic implications
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文摘

Three late Mesozoic (168–109 Ma) plutons in NW Fujian consist of I-type granites.

They exhibit variable elemental and isotopic compositions and have multiple origins.

They formed in a continental arc setting related to Paleo-Pacific plate subduction.

Progressive slab rollback is the most likely mechanism for their generation.

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