TY - JOUR
T1 - A new probe of ULVZ S-wave velocity stucture
T2 - Array stacking of ScS waveforms
AU - Avants, Megan
AU - Lay, Thorne
AU - Garnero, Edward
PY - 2006/4/16
Y1 - 2006/4/16
N2 - S-wave velocity reductions in thin layers above the core-mantle boundary (CMB) are resolved by modeling precursors to the tangential-components of core-reflected ScS phases. Unlike most phases used to study ultra-low velocity zone (ULVZ) structure, ScS provides direct sensitivity to shear velocity structure, VS. Recordings of deep earthquakes in the Tonga-Fiji and South American subduction zones at broadband seismic networks in western North America are used to map small-scale ULVZ variability. A two-layer low-VS structure exists under the central Pacific: an abrupt 0.8-2.0% decrease 60-86 km above the CMB is underlain by a 24-30 km thick ULVZ layer having reductions of 3.3-7.4% (with respect to PREM). No corresponding velocity reductions are found under the Cocos plate. The structure above the ULVZ may be associated with reverse transformation of post-perovskite to perovskite in a steep thermal gradient in a boundary layer above the CMB.
AB - S-wave velocity reductions in thin layers above the core-mantle boundary (CMB) are resolved by modeling precursors to the tangential-components of core-reflected ScS phases. Unlike most phases used to study ultra-low velocity zone (ULVZ) structure, ScS provides direct sensitivity to shear velocity structure, VS. Recordings of deep earthquakes in the Tonga-Fiji and South American subduction zones at broadband seismic networks in western North America are used to map small-scale ULVZ variability. A two-layer low-VS structure exists under the central Pacific: an abrupt 0.8-2.0% decrease 60-86 km above the CMB is underlain by a 24-30 km thick ULVZ layer having reductions of 3.3-7.4% (with respect to PREM). No corresponding velocity reductions are found under the Cocos plate. The structure above the ULVZ may be associated with reverse transformation of post-perovskite to perovskite in a steep thermal gradient in a boundary layer above the CMB.
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U2 - 10.1029/2005GL024989
DO - 10.1029/2005GL024989
M3 - Article
AN - SCOPUS:33646854256
SN - 0094-8276
VL - 33
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 7
M1 - L07314
ER -