Because of the inherent complexity of the phenomena neither cleavage nor transition cracks were geometrically characterized; however, they were localized within the cracked surface as complementary information.
Debido a la inherente complejidad de los fenómenos, ni el clivaje ni la zona de transición de la grieta se pudieron caracterizar geométricamente. Sin embargo, ambos fueron localizados dentro de la superficie fracturada como información complementaria.