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An R-Fe-B type rare earth sintered magnet in which the R2Fe14B type compound grains present at a depth of 20μm from the surface of the magnet have each an outer skin layer of (RL1-xRHx)2Fe14B (wherein 0.2≤x≤0.75) having a thickness of 1nm to 2μm (wherein RL is at least one light rare earth element selected from between Nd and Pr; and RH is at least one heavy rare earth element selected from the group consisting of Dy, Ho and Tb).