Relationship between shallow- and intermediate-depth seismicity in the eastern Aleutian subduction zone

Mathematics – Logic

Scientific paper

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Earthquakes, Seismology, Subduction (Geology), Tectonics, Aleutian Islands (Us), Geological Faults, Ray Tracing, Three Dimensional Models

Scientific paper

In order to elucidate the transition from shallow interplate thrusting to intermediate-depth seismicity, 1448 earthquakes are relocated from data recorded by a regional seismic network in the eastern Aleutian arc, using an improved 3D velocity model and accurate ray tracing. Single-event first-motion solutions are determined from these rays for 31 slab events. The interplate thrust zone is a planar fault zone, dipping 10-15 deg at 25-35 km depth, and is no more than 5-10 km wide. Fault-plane solution orientations for these events vary by several tens of degrees in orientation, although 73 percent show T axes aligned within 45 deg of the slab dip. A parallel seismic zone, 20-25 km deeper into the slab, also shows down-dip plunges of T axes for 3 of 5 solutions. Hypocenters show that intermediate-depth events are confined near the subducted oceanic crust, supporting compositional rather than pure thermal control of intermediate-depth seismicity. It is argued that the upper-plane events are an indirect consequence of phase changes in subducted crust.

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