Coseismic lateral offsets of surface rupture zone produced by the 2001 Mw 7.8 Kunlun earthquake, Tibet from the IKONOS and QuickBird imagery

Abstract

Analyses and interpretations of 1m‐resolution IKONOS, and 61cm‐resolution QuickBird images reveal that the distribution of strike‐slip offsets and ground deformation characteristics of the coseismic surface rupture produced by the 2001 M w 7.8 Kunlun earthquake occurred in the western segment of the strike‐slip Kunlun fault, northern Tibet. The 2001 coseismic strike‐slip offsets measured from IKONOS images range from 2 m up to 16.7 m, generally 3–8 m, which are generally consistent with those measured immediately in the field after the earthquake. The coseismic surface ruptures along which offsets were observed are mainly composed of a numerous of en echelon shear faults and cracks which are concentrated on a rupture zone ranging from a few meters up to ∼500 m in width. The offsets measured along individual shear faults or crack are typically 2–7 m, but up to >10 m in several locations. Our results show that high resolution remote sensing imagery provides a powerful tool for measuring coseismic strike‐slip offsets and detecting the ground deformation produced by a large earthquake in the remote and high mountain Tibet region.