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        1 - The Hiatus between the Continuous Prefix / mi-/ and Present Stem in Standard Farsi: Generative Approach
        shahin Amirjani Aliyeh  Kord Zafaranlu kambuzia Arezu Najafian
        It is important to analyze the lexicological-phonological processes of the present stem in order to evaluate the generative capacity of each phonological process. The present article aims to identify and describe the lexicological-phonological processes in simple verbs More
        It is important to analyze the lexicological-phonological processes of the present stem in order to evaluate the generative capacity of each phonological process. The present article aims to identify and describe the lexicological-phonological processes in simple verbs with the initial vowel of standard Farsi after adding the continuous prefix / mi/. The research method is descriptive-analytical. In this research, in the method of data collection, there are 50 verbs out of 323 verbal roots based on Tabataba'i (1997), Dehkhoda Dictionary (2011), and Sokhan Dictionary (2003) which begin with vowels. The data have been transcribed according to the International Phonetic Alphabet "I.P.A" and then analyzed in the framework of generative phonological theory. Results show that in written or formal Farsi, "Hamza" or the glottal stop [ʔ] is added to verbs that begin with vowel and for this reason, they begin with "A"; but after adding the continuous prefix / mi- /, "Hamza" is not inserted in the spoken or informal Farsi and instead, the front vowel shortening process, raising /i/ and gliding as short vowel sequence and gliding [-ej-] and then raising the front central vowel [e] before gliding [j] as vowel sequence and glide [-ij-] are observed. In such structures, in the informal speech, there is no "Hamza" or the glottal stop [ʔ] in the verb structure. Manuscript profile
      • Open Access Article

        2 - Balanced Cross Sections and Determine of Shortening in North Makran Ophiolite Mélange, Southeastern Iran
        Azizollah Tajvar Mohammad Mahdi Khatib Mohamad Hossian Zarinkoub
        The geometrical and kinematic characteristics of structural elements of north Makran have been measured and analyzed in five structural sections. Then, by using of balance cross sections and restoring the structures to their original state, the amount of shortening has More
        The geometrical and kinematic characteristics of structural elements of north Makran have been measured and analyzed in five structural sections. Then, by using of balance cross sections and restoring the structures to their original state, the amount of shortening has been determined in different parts of the area. The Bashagard, Dranar, Abenma, Koh Bahark and Vernach thrust faults with a WNW-ESE trend and 20 to 35 degrees dip towards the NNE are the main deformation controllers in this region and are the main cause of shortening. The excellent fit between N209/09 principal stress axis calculated based on the geometry of thrust faults and compression axis that formed folds, indicates that these structures were formed as a result of the same tectonic regime. The difference in the amount of shortening in different parts of the north Makran ophiolite mélange of is also directly related to the thrust faults. So that, in western part of north Makran, thrust faults caused shortening amount 22.66, 22.85 and 14.32% in structural sections A-A', B-B' and C-C' respectively,. In the eastern parts, due to the lack of thrust faults and the presence of more strike-slip faults, the amount of shortening has decreased to 4.52% and 6.67%, respectively, in the sections D-D' and E-E'. Balanced cross sections and restoring the structures to the pre-deformation stages represent the narrow width of the early oceanic basin in the north of Makran. Manuscript profile