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

Journal Article · · Geophysical Research Letters (American Geophysical Union); (United States)
DOI:https://doi.org/10.1029/92GL02060· OSTI ID:5145942
 [1]
  1. Columbia Univ., Palisades, NY (United States)
The transition from shallow interplate thrusting to intermediate-depth seismicity is often poorly observed, but critical for understanding the fate of the downgoing slab. In order to better examine the transition, 1448 earthquakes are relocated from data recorded by a regional seismic network in the eastern Aleutian arc, using an improved three-dimensional 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[degrees] at 25-35 km depth, and is no more than 5-10 km wide. Most intermediate-depth earthquakes are localized to a plane no wider than 5 km near the top of the descending plate. Fault-plane solution orientations for these events vary by several tens of degrees in orientation, although 73% show T axes aligned within 45[degrees] 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 to 5 solutions. The fault-plane solutions are poorly explained by plate bending ur unbending about a neutral fiber. Hypocenters show that intermediate-depth events are confined near the subducted oceanic crust, supporting compositional rather than pure thermal control of intermediate-depth seismicity. One explanation is that the upper-plane events are an indirect consequence of phase changes in subducted crust. Perhaps similar processes are important in producing earthquakes in the lower, parallel zone. 26 refs., 4 figs.
DOE Contract Number:
FG02-84ER13221
OSTI ID:
5145942
Journal Information:
Geophysical Research Letters (American Geophysical Union); (United States), Journal Name: Geophysical Research Letters (American Geophysical Union); (United States) Vol. 19:20; ISSN GPRLAJ; ISSN 0094-8276
Country of Publication:
United States
Language:
English