HR: 0830h
AN: G21B-0267 [PDF]
TI: Imaging depth variations of interplate coupling
AU: * Aoki, Y
EM: aoki@ldeo.columbia.edu
AF: Lamont-Doherty Earth Observatory of Columbia University, P.O. Box 1000, Route 9W, Palisades, NY 10964 United States
AU: Scholz, C H
EM: scholz@ldeo.columbia.edu
AF: Lamont-Doherty Earth Observatory of Columbia University, P.O. Box 1000, Route 9W, Palisades, NY 10964 United States
AB:
Recent geodetic measurements have revealed that brittle-plastic
transition zones (BPTZs) are loci of slow slip episodes.
Furthermore, recent seismic observations detected non-volcanic harmonic
tremors at the BPTZ. It is important to estimate the depth range of
BPTZs and how interplate coupling changes within the BPTZ, not only
for understanding the interseismic stress accumulation process
in subduction zones but also exploring the causes of slow
slip and harmonic tremors. Here we imaged depth variations of
interplate coupling in the Nankai trough, southwest Japan, by
inverting Global Positioning System (GPS) velocities to gain more
insight into the rheology of the BPTZ in subduction zones.
Interplate coupling was estimated for three profiles: the source
region of the 1946 Nankaido earthquake, that of the 1944 Tonankai
earthquake, and the Tokai seismic gap. The results show a gradual
decrease of interplate coupling between about 20-25 and 35-45 km
depth with a plateau region between 25-35 km for all three profiles.
Because there are GPS sites near the trench, the Tokai profile was
capable of resolving interplate coupling at shallower depths than
the other two profiles. The result from the Tokai profile shows that
interplate coupling decreases from full to zero above 6 km depth.
The updip limit of the seismogenic zone for the Tokai profile is
significantly shallower than expected for the Nankaido profile,
consistent with seamount subduction under the accretionary
prism.
DE: 1243 Space geodetic surveys
DE: 7218 Lithosphere and upper mantle
DE: 8150 Plate boundary--general (3040)
DE: 8159 Rheology--crust and lithosphere
DE: 9320 Asia
SC: Geodesy [G]
MN: 2003 Fall Meeting