Факультет біології, географії та екології
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Item ЭВОЛЮЦИЯ РЕЛЬЕФА ПАМИРА И ГИССАРО-АЛАЯ В ФАНЕРОЗОЕ(2010) Винниченко, Г. П.; Таджибеков, М.; Vinnichenko, G.P.; Tojibekov, M.Each of stages of the geological evolution of Pamir and Hissar - Alay in the Phanerozoic was characterized by ал originality of the relief, which has generated in these stages. The changes of the relief occurred 011 the background of its general evolution, expressed in the strengthening o f contrast and ruggedness of the land surface.Item ПРИНЦИП УНАСЛЕДОВАННОСТИ И ОСОБЕННОСТИ ФОРМИРОВАНИЯ ВНУТРИГОРНЫХ ВПАДИН В НОВЕЙШЕМ ЭТАПЕ (НА ПРИМЕРЕ ГИССАРО-АЛАЯ И ПРИЛЕГАЮЩИХ ТЕРРИТОРИЙ)(2009) Винниченко, Г. П.; Таджибеков, М.; Vinichenko, G. P.; Tojibekov, M.Use of a principle of hereditary in the analysis of a history of formation intermountain hollows Hissar-Alay region and adjacent territories has given new confirmations on necessity ложения of a situation of the bottom border of the newest stage up to a sole Pleistocene.Item ПАЛЕОСЕЙСМОДИСЛОКАЦИИ И ПРИРОДА СВЯЗЕЙ ОЧАГОВ СЕЙСМИЧЕСКИХ ТОЛЧКОВ С ДИЗЪЮНКТИВАМИ(2008) Винниченко, Г. П.; Таджибеков, М.; Vinichenko, G. P.; Tojibekov, M.The carried out researches show, that to the seismodangerous areas should not belong onl> fault zones, (mainly in connection with their adverse engineering-geological conditions), but also significant space between fault zones. In last occurs significant accumulation of the seismogeneraiing straining.