Late Silurian-early Devonian adakitic granodiorite, A-type and I-type granites in NW Junggar, NW China: Partial melting of mafic lower crust and implications for slab roll-back
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文摘
The intrusions in NW Junggar were emplaced during 420–405 Ma. The intrusions were likely formed by partial melting of mid-lower crust. A slab roll-back was probably existed in late Silurian–early Devonian in NW Junggar.
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