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Hydrated Peridotite – Basaltic Melt Interaction Part I: Planetary Felsic Crust Formation at Shallow Depth

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Academic year: 2021

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FIGURE 1 | Upper panel: Scheme of time-series runs at 0.2 GPa, showing starting con fi gurations and fi nal products containing felsic glasses
TABLE 1 | Experimental run conditions and the resulting phases with the phase proportions.
FIGURE 2 | Backscattered electron images and elemental X-ray maps of the hybrid and mixed runs to investigate aqueous fl uid-assisted partial melting of peridotite at pressures of 0.2 and 0.5 GPa
FIGURE 3 | (A) Phase compositions plotted as serpentine (SERP) proportion (in wt%) vs
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