ЭВОЛЮЦИЯ РЕЛЬЕФА ПАМИРА И ГИССАРО-АЛАЯ В ФАНЕРОЗОЕ

dc.contributor.authorВинниченко, Г. П.
dc.contributor.authorТаджибеков, М.
dc.contributor.authorVinnichenko, G.P.
dc.contributor.authorTojibekov, M.
dc.date.accessioned2017-05-18T11:49:51Z
dc.date.available2017-05-18T11:49:51Z
dc.date.issued2010
dc.descriptionВинниченко, 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.uk_UA
dc.description.abstractEach 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.uk_UA
dc.identifier.urihttp://ekhsuir.kspu.edu/handle/123456789/2821
dc.subjectevolutionuk_UA
dc.subjectreconstructionuk_UA
dc.subjectdiastrophismuk_UA
dc.subjectdepressionuk_UA
dc.subjectsedimentationuk_UA
dc.subjectgeoteclonic regimeuk_UA
dc.subjectPamiruk_UA
dc.subjectTian-Shanuk_UA
dc.titleЭВОЛЮЦИЯ РЕЛЬЕФА ПАМИРА И ГИССАРО-АЛАЯ В ФАНЕРОЗОЕuk_UA
dc.title.alternativeTHE RELIEF EVOLUTION OF PAMIR AND HISSAR-ALAY IN THE PHANEROZOICuk_UA
dc.typeArticleuk_UA

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