High-precision teleseismic double-difference locations and focal mechanisms of aftershocks of the A.D. 2004 Mw 9.2 Sumatra-Andaman earthquake illuminate an active imbricate fault system in the accretionary prism offshore northern Sumatra. They reveal repeated failure of a shallow northeast-dipping thrust fault above the megathrust, which we interpret to be the reactivation of a splay fault that rises from the megathrust at ~55 km depth and cuts through the overriding Sunda plate. The projected intersection of the splay fault with the seafl oor correlates with a recently active thrust fault seen in postseismic bathymetry data west of the Aceh basin. A spatiotemporal analysis of the streaky aftershock distribution indicates that ascending fl uids released from the subducting oceanic crust along inherited seafl oor fabric may control brittle fracture in the overriding plate. We speculate that if the splay fault was active coseismically, it may have led to amplifi ed vertical uplift of the forearc ridge and contributed to generating the cataclysmic near-fi eld tsunami that struck the northwest Sumatra coast following the 2004 rupture.
Splay faults imaged by fluid-driven aftershocks of the 2004 Mw 9.2 Sumatra-Andaman earthquake
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