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- W2023890163 abstract "article The mantle source of late Mesozoic mafic magmas in the southeastern North China Craton is generally con- sidered to have been enriched by deeply subducted continental lithosphere of the Yangtze Block. The mechanisms through which enrichment occurs are still unclear. Here we document an Early Cretaceous (zircon U-Pb age at 115 ± 2 Ma) dioritic intrusion with some geochemical features similar to sanukitoids (i.e., Al2O3 N 17.5%, Ba = 1692-1819 ppm, Sr = 1042-1111 ppm and δ 18 OZircon =6 .2 ± 0.2‰ )f rom the Sulu Orogen in North China. Compared with the regional older (120-130 Ma) mafi cm agmas (dykes), the diorite has less radiogenic Sr ( 87 Sr/" @default.
- W2023890163 created "2016-06-24" @default.
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- W2023890163 date "2014-08-01" @default.
- W2023890163 modified "2023-10-16" @default.
- W2023890163 title "Hf–Nd–O isotopic evidence for melting of recycled sediments beneath the Sulu Orogen, North China" @default.
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- W2023890163 doi "https://doi.org/10.1016/j.chemgeo.2014.04.028" @default.
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