Extended Data Fig. 4: Diagrams of whole-rock 87Sr/86Sr(i) and \({\boldsymbol{\mathcal{E}}}_{{\bf{Nd}}}({\bf{t}})\) values versus SiO2 contents for Late Cretaceous-Early Cenozoic magmatic rocks from the Gangdese arc. | Nature

Extended Data Fig. 4: Diagrams of whole-rock 87Sr/86Sr(i) and \({\boldsymbol{\mathcal{E}}}_{{\bf{Nd}}}({\bf{t}})\) values versus SiO2 contents for Late Cretaceous-Early Cenozoic magmatic rocks from the Gangdese arc.

From: India–Eurasia convergence speed-up by passive-margin sediment subduction

Extended Data Fig. 4

Samples from the literature do not exhibit negative or positive covariation patterns between whole rock 87Sr/86Sr(i), \({{\mathcal{E}}}_{{\rm{Nd}}}({\rm{t}})\) values, and SiO2 contents.

Source Data

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