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A fundamental debate exists regarding the geometry and depth extent of seismogenic faults in eastern Tibet. Along the Longmen Shan, geologic and seismic reflection data reveal a belt of low to moderate angle thrust faults, some of which may have been activated in devastating earthquakes in 2008 (Mw ∼7.9, Wenchuan) and 2013 (Mw ∼6.6, Lushan). However, geologic and geodetic constraints on these ruptures...
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