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Slip-Rate Measurements on the Karakorum Fault May Imply Secular Variations in Fault Motion Export

Science, Vol. 307, No. 5708. (21 January 2005), pp. 411-414.

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cosmogenic secular_variation slip_rate

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Beryllium-10 surface exposure dating of offset moraines on one branch of the Karakorum Fault west of the Gar basin yields a long-term (140- to 20-thousand-year) right-lateral slip rate of [~]10.7 +/- 0.7 millimeters per year. This rate is 10 times larger than that inferred from recent InSAR analyses ([~]1 +/- 3 millimeters per year) that span [~]8 years and sample all branches of the fault. The difference in slip-rate determinations suggests that large rate fluctuations may exist over centennial or millennial time scales. Such fluctuations would be consistent with mechanical coupling between the seismogenic, brittle-creep, and ductile shear sections of faults that reach deep into the crust. 10.1126/science.1105466


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