ЭВОЛЮЦИЯ РЕЛЬЕФА ПАМИРА И ГИССАРО-АЛАЯ В ФАНЕРОЗОЕ

Abstract

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.

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Винниченко, Г. П. ЭВОЛЮЦИЯ РЕЛЬЕФА ПАМИРА И ГИССАРО-АЛАЯ В ФАНЕРОЗОЕ / Г.П.Винниченко, М.Таджибеков // ДОКЛАДЫ АКАДЕМИИ НАУК РЕСПУБЛИКИ ТАДЖИКИСТАН. - 2010. - Том 53, №11. - С. 879-882.

Keywords

evolution, reconstruction, diastrophism, depression, sedimentation, geoteclonic regime, Pamir, Tian-Shan

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