Late Neoarchean subduction-related crustal growth in the Northern Liaoning region of the North China Craton: Evidence from ∼2.55 to 2.50 Ga granitoid gneisses
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文摘

Voluminous ∼2559–2495 Ma granitoid gneisses in Northern Liaoning, NCC.

Quartz dioritic to TTG gneisses stemmed from juvenile basaltic rocks.

Potassium-rich granitoids sourced from metasomatized mantle or metagreywackes.

A late Neoarchean (∼2.6–2.5 Ga) arc–continent accretion system.

Significant late Neoarchean crustal growth of the NLP and the entire NCC.

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