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25 April 2024
 
  » pubmed » pmid15662010

 Article overview



Slip-rate measurements on the Karakorum Fault may imply secular variations in fault motion
M-L Chevalier ; F J Ryerson ; P Tapponnier ; R C Finkel ; J Van Der Woerd ; Li Haibing ; Liu Qing ;
Date 21 Jan 2005
Journal Science, 307 (5708), 411-4
AbstractBeryllium-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 approximately 10.7 +/- 0.7 millimeters per year. This rate is 10 times larger than that inferred from recent InSAR analyses ( approximately 1 +/- 3 millimeters per year) that span approximately 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.
Source PubMed, pmid15662010 doi: 10.1126/science.1105466
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