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A series of rare-earth phosphates, arsenates, vanadates, tantalates and niobates have been reacted at pressures up to 80,000 atm. and temperatures up to 600°C. The structures of the high-pressure phases “quenched” to ambient conditions have been evaluated by x-ray powder diffractometry.

High-pressure scheelite-structure polymorphs of rare-earth vanadates and arsenates