The pseudocubic martensite (Fe-C alloy) is typically described as tetragonal phase. Why space group type P 42/n (IT-Nr. 86) is used?
I 4/mmm would generate the same atomic arrangement, and also P 42 (but with a shift of the origin.
A further problem is that martensite is often understood as a carbon layered structure. However, if P 42/n is used, does this really describes a layering perpendicular to c?