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• W2037505095 abstract "The North China and Yangtze blocks collided in the Triassic in central Eastern China (e.g., Li et al., 2000), forming the Dabie–Sulu orogen with an over-thickened crust similar to the one beneath the present Himalaya. Results of seismological studies indicate that the current crustal thickness of the Dabie–Sulu orogen is about 35 km (Wang et al., 2000; Sodoudi et al., 2006), indicating that a significant amount of mountain root of this orogen was removed and recycled into the convective upper mantle. The foundering mechanism of the eclogitic lower crust of the Dabie–Sulu orogen is still poorly understood. Studies on the post-collisional igneous rocks from the Dabie–Sulu orogen have provided important constraints on the timing and processes of mountain root removal as well as lithospheric thinning of central China (Wang et al., 2007; Xu et al., 2007; Huang et al., 2008; Zhang et al., 2010). In a recent study, Zhang et al. (2010) reported high quality geochronological and geochemical data for the Meichuan pluton from the Southern Dabie orogen and suggested that the Meichuan pluton is a high-Mg adakite formed during the early Cretaceous. However, these authors believed that “high-Mg adakites have not been found" @default.
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• W2037505095 date "2011-07-01" @default.
• W2037505095 modified "2023-09-24" @default.
• W2037505095 title "Comment on “Origin of high-Mg adakitic magmatic enclaves from the Meichuan pluton, southern Dabie orogen (central China): Implications for delamination of the lower continental crust and melt–mantle interaction” by C. Zhang, C.Q. Ma, F. Holtz [Lithos 119 (2010) 467–484]" @default.
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• W2037505095 doi "https://doi.org/10.1016/j.lithos.2010.10.018" @default.
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