Constraints of volcanic rocks of the Wutai Complex (Shanxi Province, Northern China) on a giant late Neoarchean intra-oceanic arc system in the Trans-North China Orogen
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文摘

Wutai meta-volcanics erupted from 2548 Ma to 2538 Ma.

Xenocrystic zircons at 3.61 Ga, 2.97–2.83 Ga and 2.7 Ga were found.

Group 1 derived from partial melting of depleted mantle in a fore-arc tectonic setting.

Group 2 and 3 derived from a metasomatized mantle wedge.

An intra-oceanic arc underlain in part by a ∼2.7 Ga micro-continent at 2.55–2.52 Ga.

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