Teleseismic Shear-Wave Splitting


(Above) Average fast axis orientation and lag time for teleseismic phases for each
station of the CHARGE network and GEOSCOPE station PEL. From Anderson
et al. (2004), Geophysical Research Letters.

Though subduction has long been explored as a kinematic
phenomenon, our understanding is still incomplete. We have
an even more limited understanding of subduction dynamics.
Subduction kinematics and dynamics has largely been explored
with numerical modeling, and validation of existing
subduction models still needs to be made with new data.
Mantle flow patterns interpreted from seismic anisotropy can
serve as such a validation. In my thesis work, I have been
using data collected in 2000-2002 as a part of the CHARGE
(Chile Argentina Geophysical Experiment) Passcal seismic
deployment to analyze shear-wave splitting from both
teleseismic and local s-waves. I am using these measurements
to determine seismic fast direction both above and below the
subducting slab in the South American subduction zone of
Chile and Argentina, and from these observations, infer
mantle strain and potential patterns of mantle flow. The
station distribution in our study is such that we can see a
change in seismic fast direction over several measurements
across a slab-dip transition: the subducting slab dip changes
along strike, from nearly flat in the north to normally-
dipping in the southern part of our field area. The most
important result so far is a correlation of seismic fast
direction with slab geometry both above and below the slab.
This observation demonstrates that the change in slab dip is
likely affecting either mantle rheology, strain pattern, or
both and therefore affecting mantle flow in a direction not
parallel to either the direction of slab dip or strike of the
trench. Such 3-D mantle flow, rheology, and dynamics could
affect the path and nature of fluid fluxes through the mantle
wedge, interaction of asthenospheric flow below the slab with
deeper patterns of mantle convection, and the nature of
deformation of the overriding crust through its interaction
with flow (or lack of flow) in the mantle wedge.

Publications and Recent Abstracts

Anderson, M. L., Zandt, G., Triep, E., Fouch, M., Beck, S., 2004, Anisotropy and mantle flow in the Chile-Argentina
subduction zone from shear wave splitting analysis: Geophysical Research Letters, 31, L23608,
doi:10.1029/2004GL020906, (316 KB).

Anderson, M. L., Zandt, G., Triep, E., 2004, Mantle flow in the Chile-Argentina flat slab subduction zone from seismic
anisotropy: 16th Annual IRIS Workshop, (Page Size Poster 1.1 MB).

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Last Updated: 01/2005