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We report the microstructures of two different groups of recovered samples from natural peridotite KLB-1: one has gone through partial melting at 1.5GPa, and the other group has gone through a solid phase transition from spinel peridotite to garnet peridotite at 5GPa. Static melting in the KLB-1 sample is dominated by grain boundary melting for times less than 1min. The melt evolves to the triple...
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