coarse-grained magnesium alloy, with an average grain size of∼ 50 µm, and a low fracture
toughness. The results show that {10 1 2}-type deformation twins are formed at the crack tip
and many dislocations pile up on these boundaries. The accumulated strains at these
boundaries become the origin of fracture; ie cracks propagate along these boundaries
between the deformation twins and the matrix.