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. 2021 Jul 14;12:4311. doi: 10.1038/s41467-021-24533-7

Fig. 3. Heterogeneity of subduction zone compositions and processes.

Fig. 3

Differences in water2 (a) and carbon3,4 (b) flux among subduction zones and corresponding C recycling efficiency (c). The water flux estimates assume moderate mantle hydration2.