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The Tian Shan, east-west trending more than 2000 km, is one of most active intracontinental mountain building belts that resulted from India-Eurasia collision during Cenozoic. In this study, Quaternary folding related to intracontinental mountain building of the Tian Shan orogenic belt is documented based on geologic interpretation and analyses of the satellite remote sensing images [Landsat Thematic...
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