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False-color, three-dimensional density map of a sample of pelitic schist from British Columbia, Canada, generated from high-resolution computed x-ray tomography images. The sizes and relative positions of the large garnet crystals (red orbs) provide clues about the atomic-scale mechanisms that govern metamorphic recrystallization. See page 1236. [Image: Cambria Denison]


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Science. ISSN 0036-8075 (print), 1095-9203 (online)