Fig. 5.
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Silicate grain shape evolution for the simulation of pyroxenic composition at 600 K pyroxenic composition at 1100 K, olivinic composition at 600 K and olivinic composition at 1100 K (from top to bottom). The black circle indicates the ratio defining a perfect sphere. The grey dashed line corresponds to the cases in which grains would be equally prolate and oblate. The results were obtained as the average over ten NAGGS runs.
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