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Fig. 12 | Progress in Earth and Planetary Science

Fig. 12

From: Geochemical characteristics of back-arc basin lower crust and upper mantle at final spreading stage of Shikoku Basin: an example of Mado Megamullion

Fig. 12

Bulk compositional variation between MORB-normalized (MORB-N) Yb and MgO. Modeled melting trends during fractional and incremental batch melting of fertile mantle peridotite in the garnet stability field and spinel stability field are modified after Yoshikawa and Nakamura (2000). Abbreviations: Du = dunite, and Pe = peridotite

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