“…It can be expected that the dynamic theory of dislocations will be an appropriate means to calculate these waves and to determine the parameters of their source by analysis of the waves. This was done for seismic sources such as faults [2], and, at the microscopic scale, for acoustic emission sources such as dislocations, microcracks, local creation of free surfaces by shear (denoted here by shear decohesion) [3,4,5,6,7,8,9], and local formation of a new phase [10].…”