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EW-trending uplifts along the southern side of the central segment of the Altyn Tagh Fault, NW China: Insight into the rising mechanism of the Altyn Mountain during the Cenozoic

GeophysicsEngineeringGeographyAltyn MountainGeologyAltyn Tagh FaultNw ChinaRegional TectonicsOrogenyNeotectonicsEarth ScienceMountain UpliftTectonics