Late Quaternary and present‐day rates of slip along the Altyn Tagh Fault, northern margin of the Tibetan Plateau

Both Global Positioning System (GPS) measurements and studies of Late Quaternary faulting are consistent with a slip rate of ∼10 mm/yr along the central segment of the Altyn Tagh Fault and a systematic decrease in that rate toward the eastern end of the fault. Dates of terraces above and below later... View More