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Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF, file size: 1132870 bytes)
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 111,
B05305,
doi:10.1029/2004JB003270,
2006
Shear velocity variation within the D″ region beneath the central Pacific
Megan Avants
Earth Sciences Department, University of California, Santa Cruz, California, USA
Thorne Lay
Institute of Geophysics and Planetary Physics, University of California, Santa Cruz, California, USA
Sara A. Russell
Weston Geophysical Corporation, Lexington, Massachusetts, USA
Edward J. Garnero
Department of Geological Sciences, Arizona State University, Tempe, Arizona, USA
Abstract
Small-scale variability of shear velocity (Vs) structure in the D″ region beneath the central Pacific is imaged using 442 broadband tangential component S waveforms recorded in western North America for 37 intermediate and deep focus Tonga-Fiji earthquakes. Double-array stacking
of spatially binned subsets of data reveals lateral variations in the relative timing and amplitude of deep mantle discontinuity
reflections on scale lengths of about 130 km across the ∼6° × 8° region of D″ sampled. Waveform modeling using localized one-dimensional
structures indicates variations of the Vs increase at the D″ discontinuity ranging from 0.5% to 2.3%, and discontinuity depths ranging from 2490 to 2735 km, deepening
and weakening from southwest-to-northeast across the study area. Two abrupt Vs reductions are also detected within the D″ layer. We thus present a laterally variable three-layer model of the D″ region
beneath the central Pacific. The complex structure may be associated with lateral thermal and chemical gradients that produce
a lens of postperovskite material above an ultralow-velocity zone on the margin of a large low shear velocity province.
Received 28
June
2004;
accepted 24
January
2006;
published 4
May
2006.
Keywords: D″;
core mantle boundary;
deep mantle.
Index Terms: 7203 Seismology: Body waves; 7208 Seismology: Mantle (1212, 1213, 8124); 8120 Tectonophysics: Dynamics of lithosphere and mantle: general (1213); 8121 Tectonophysics: Dynamics: convection currents, and mantle plumes; 8124 Tectonophysics: Earth's interior: composition and state (1212, 7207, 7208, 8105).
Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF, file size: 1132870 bytes)
Citation: Avants, M., T. Lay, S. A. Russell, and E. J. Garnero
(2006),
Shear velocity variation within the D″ region beneath the central Pacific,
J. Geophys. Res.,
111,
B05305,
doi:10.1029/2004JB003270.
Copyright 2006 by the American Geophysical Union.
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