Abstract:The discrepant arrangement of the Carpathian nappes and syntectonic deposits of the Carpathian Foredeep reveals the oroclinal migration of the subduction direction of the platform margin during the Late Cenozoic. Formation of the nappes was induced by their detachment from disintegrated segments of the European Platform; the segments were shortened as a result of their vertical rotation in zones of compressional sutures. It finds expression in local occurrence of the backward vergence of folding against the generally forward vergence toward the Carpathian Foredeep. The precompressional configuration of sedimentation areas of particular nappes was reconstructed with application of the palinspastic method, on the basis of the hitherto undervalued model which emphasizes the influence of the subduction and differentiated morphology of the platform basement on the tectonic evolution of the fold and thrust belt. Superposition of the palaeogeographic representations and the present geometry of the orogen allows understanding of the impact of the magnitudes of tectonic displacements on the differentiation of the geological structure in the NE segment of the Carpathians. The differentiation has inspired different views of Polish and Ukrainian geologists on structural classification and evolution of the frontal thrusts.

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The borrowing process of Italianisms and Venecianisms in Croatian Čakavian local languages of DalmatiaItalian and Venetian loanwords in the territory of Dalmatia were the result of complex, lengthy and intensive contacts, first Croatian-Romanian and later Croatian-Italian. In Dalmatia these are the Roman languages which have clearly indicated their presence in vocabulary and numerous works of linguists and dialectologists were devoted to this phenomenon. Apart from linguistic sources, also the historical ones inform us about multiculturalism and bilingualism, which developed in the Dalmatian cities. The outcomes of language contacts are numerous linguistic borrowings from Italian and Venetian dialect in Čakavian lexical system. The adaptation process of Venetian and Italian borrowings occurs at the phonological, morphological and semantic level. This article describes only the adaptation at the morphological and linguistic level in the language system of Čakavian dialect. It should be noted, however, that a linguistic borrowing is adapted at the phonological level first. As it is clear from the material discussed, a linguistic borrowing goes through three phases of transmorphemisation. At the formative level, Čakavian lexical system was enriched by new suffixes. At the semantic level, we can see that a borrowing in the recipient language retains the original meaning, there is also an expansion or a narrowing of the meaning compared to the one of the donor language. The most productive class of borrowed words are nouns, verbs are more rarely borrowed, as well as adjectives, adverbs, prepositions and interjections. It seems that the cause of the advantage of nouns borrowed over other parts of speech lies in their semantics.