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The Tarim Basin in western China has been receiving continuous marine to lacustrine deposits during the Cenozoic as a foreland basin of the Qinghai–Tibetan Plateau (QTP). Clay mineralogy and geochemical proxy data from these sedimentary archives can shed light on climate and tectonic trends. Here we report on an abrupt mineralogical and weathering shift at 17 Ma ± 1 Myr in the Miocene Qimugan section...
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