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Detailed Reference Information |
Park, J., Yuan, H. and Levin, V. (2004). Subduction zone anisotropy beneath Corvallis, Oregon: A serpentinite skid mark of trench-parallel terrane migration?. Journal of Geophysical Research 109: doi: 10.1029/2003JB002718. issn: 0148-0227. |
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We studied the back azimuth dependence of Ps converted phases at GSN station COR (Corvallis, Oregon) using broadband P receiver functions computed from 602 teleseismic earthquakes. The amplitudes and polarities of the transverse Ps phases are largely two-lobed, which indicates anisotropy with a tilted symmetry axis. A double-peaked Ps conversion at 4.5--6.5 s delay has the moveout of a dipping slab but is not consistent with simple deflection of the Ps converted phase by the dipping interface. A polarity flip on the transverse receiver function near north-south back azimuth indicates an anisotropic symmetry axis aligned north-south, far from the convergence direction (N68¿E). The Ps phase is modeled using reflectivity synthetics with a highly anisotropic layer of depressed wave speed (VP ~ 6.0--6.5 km/s) near 40 km depth, at the slab interface with the overriding North American plate. One-dimensional modeling suggests 10% anisotropy in the supraslab layer, with a slow symmetry axis oriented N5¿W at a 60¿ tilt from the vertical. Adjustments for the effect of slab interface dip on Ps amplitude suggest a somewhat lower 7% anisotropy. We infer a thin (~7 km) anisotropic detachment zone for the northward slippage of the Siletz forearc terrane along the top of the descending slab, a motion consistent with GPS measurements and models of regional lithospheric dynamics. Serpentinite is a likely constituent for the deep anisotropic layer, owing to its reduced VP and high Poisson ratio. The ductile rheology and hydrated composition of serpentinite make it a plausible lithology for a mechanical detachment zone. |
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Abstract |
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Keywords
Mineral Physics, Elasticity and anelasticity, Seismology, Body wave propagation, Seismology, Lithosphere and upper mantle, Tectonophysics, Plate boundary—general, Tectonophysics, Rheology—crust and lithosphere, anisotropy, Cascadia, subduction |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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