SINTERED BODY FOR FORMING RARE EARTH MAGNET, AND RARE EARTH SINTERED MAGNET

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A novel, hitherto unseen rare earth sintered magnet which has both remarkably low carbon content and an extremely small average particle diameter of magnet material particles, and a sintered body for forming such a magnet, are provided. This sintered body for forming a rare earth magnet is configured by sintering into a single body a plurality of magnet material particles containing a rare earth material and each having an easy magnetization axis. This sintered body for forming a rare earth magnet has a carbon content of less than or equal to 500 ppm, and moreover, the average particle diameter of the magnetic material particles is less than or equal to 2 μm.