Although geodetic measurements of interseismic deformation in interior Tibet suggest slow
strain accumulation, active slip along the right-lateral Gyaring Co Fault is suggested to be between 8
and 21 mm/yr. Reliable geologic constraints on the slip rate along this fault are sparse. Here we document
12 ± 2 m of...
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, central Tibet
Holocene slip rate along the Gyaring Co Fault, central Tibet
Shi, X., Kirby, E., Lu, H
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