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The NE Tibetan Plateau has become an important region for deciphering the Cenozoic uplift of the Plateau. Previous studies have verified that the Quaternary uplift in this region had a multi-stage character; however geologists have not established which event constituted the main tectonic phase. Fortunately, stratigraphic and paleomagnetic evidence from the Jiuquan Basin, Gansu Province, China, now...
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