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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...
Late Quaternary right-lateral displacement and slip rates have been determined along WNW-ESE-trending active faults in the intermontane Yanqi Basin on the southeastern flank of the Chinese Tian Shan. Detailed analyses of satellite images and field investigation have revealed that the active Kaidu River fault zone on the southern margin of the basin is a strike-slip fault zone. Drainage systems incising...
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