Age and geochemistry of the early Mesoproterozoic A-type granites in the southern margin of the North China Craton: Constraints on their petrogenesis and tectonic implications
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文摘

The Zhangjiaping pluton in the southern margin of the NCC was emplaced at ca. 1.53 Ga.

These granites show an affinity to fractionated aluminous A-type granites.

They originated from partial melting of the Archean calc-alkaline granitoids.

They were the products of anorogenic magmatism.

Their generation was related to the breakup of the Columbia supercontinent.

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