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Garnet amphibolite as relics of TTG magma: Evidence from the Wuhe complex in the eastern North China Craton
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DOI：10.1016/j.lithos.2026.108704.png)
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Abstract
En 中文
• Direct field evidence from Wuhe amphibolites identifies TTG magma residues. • Thermodynamic modelling confirms TTG melt generation at ∼840 °C and ∼ 9 kbar via amphibolite anatexis. • Melt compositions reflect both protolith heterogeneity and P–T controlled residual mineralogy.
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