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The Inner Mongolian Plateau, along the southeastern flank of the wider Mongolian Plateau, is a vast undulating surface ranging in elevation between 900 and 1500m above sea level. The peculiar topography of this area is assumed to be closely related to its complex tectono-thermal evolution since Late Paleozoic. The lithospheric structure of the Plateau includes three continental blocks: the Mandula...
Since the Cenozoic, the Tian Shan is rejuvenated by crustal shortening related to the ongoing India–Asia collision. However, the tectonic process prior to the Cenozoic remains ambiguous, especially in the Bogda area of the eastern Tian Shan. The continuous Late Paleozoic–Mesozoic sequences in the Bogda area record abundant information about the basin–mountain interaction. U–Pb (LA–ICP-MS) dating of...
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