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Tectonic and sedimentary evolution of the late Miocene–Pleistocene Dali Basin in the southeast margin of the Tibetan Plateau: Evidences from anisotropy of magnetic susceptibility and rock magnetic data

EngineeringRock Magnetic DataTectonic EvolutionEast Asian LanguagesGeologySedimentary EvolutionGeochronologyEarth ScienceTibetan PlateauTectonics