Purpose The purpose of this study is to investigate the mechanisms of degradation of aluminum metallization under conditions of thermal shock caused by rectangular current pulses (amplitude j < 8 × 1010 A/m2, duration t < 800 μs). Design/methodology/approach The results were obtained using oscillography and optical microscopy and through the construction of an empirical model of the thermal degradation of metallization systems. Findings Initially, for the authors’ studies, they deduced an equation that associated the depth of melting with the parameters of a current pulse. Research limitations/implications The authors were able to observe effects only in systems with appropriate adhesion of the thin metal films. For the systems with bad adhesion, the main mechanisms of degradation were associated with the melting of the metal, the formation of melted drops (up to 20 mcm in size) and the movement of these drops along the electrical field due to the electrocapillary effect. Practical/implications The mechanisms the authors studied could only occur in high-power semiconductor devices. Originality/value The principal mechanism of melting of a metallization track is linked to the heat dissipation at the interface of solid and liquid phases under conditions of thermal shock. The authors estimated the mechanical stresses in subsurface layers of silicon in the proximity of a non-stationary thermal source. The authors’ results show that the mechanical stresses that are strong enough to form dislocations emerge with current flow with power measuring approximately 0.7 Pkr.

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Previously unknown exoskeletal plates of certain Middle Devonian psammosteids, i.e., Pycnos teus palaeformis Preobrazhensky, Psammolepis proia Mark Kurik, and Schizosteus (?) sp., from localities of the Aruküla Regional Stage of the eastern part of the Main Devonian Field (Leningrad Region, Russia) are described. The psammosteid Schizosteus (?) sp. described in open nomenclature in connection with the absence of well preserved median plates has only been found in several localities (Zaitsevo, Siverskii, and Bel ogorka). The shape of the branchial plate of Tartuosteus giganteus (Gross) and ventral plate of Psammolepis proia is specified. The psammosteid Psammolepis proia from the eastern part of the Main Devonian Field is described for the first time.

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