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452                        M. WEICK AND 1 AKTAA

            The fractographic analyses of the rupture surface with a scanning electron microscope revealed
            areas with distinct oscillation lines. The orientation of the oscillation lines in the different areas
            varied. Hence a multiple redirection of  the crack can be assumed. The varying width of  the
            oscillation lines corresponds well with the assumption of varying crack growth rates. Between
            the areas with  oscillation lines, regions with  a noticeable brittle fracture proportion and no
            oscillation lines could be observed. In cause of  this unequal distribution of  the striations it is
            not clear how to determine the crack growth rate our of the striation wide. In a further step an

























                   c
                                                             6

                                        Fig. 10. Fracture surface




























                                        Fig. 11. Fracture surface
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