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贝氏体的表面凹凸定义的各个方面

Criticismsofreportsthatferritelathshaveasessileinterfacialstructurearerefuted.A locallatticecorrespondence, achievedacrosscoherentregionsbetweeninterfacialdefects,sufficestoproduce surfacereliefsandmartensiticcrystallography [Prog.Mater.Sci.42(1997)101].However,formationoftent-shapedsurfacereliefsby monocrystalline laths/platesisinconsistentwithmartensiticgrowth.

贝氏体的表面凹凸定义的各个方面

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