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3D seismic imaging of the earth’s mantle. Barbara Romanowicz Department of Earth and Planetary Science U.C. Berkeley. Surface waves. Loma Prieta (CA) 1989 M 7 earthquake observed at KEV, Finland. Surface waves. Surface waves. SS. S. P. P. Global Transverse Component Stacks.
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3D seismic imaging of the earth’s mantle Barbara Romanowicz Department of Earth and Planetary Science U.C. Berkeley
Loma Prieta (CA) 1989 M 7 earthquake observed at KEV, Finland Surface waves Surface waves SS S P P
Global Transverse Component Stacks Shearer, 1991
Sumatra 12/26/04 M9.3 (0.8 to 2.2 mHz) CAN 1S5 3S2 1S4 UNM 0S12 0S9 0S8 0S13 0S7 0S10 0S0 0S11 0S5 0S5 1S3 /3S1 0S6 mHz x10 200 hours starting 10 hours before origin time
PRELIMINARY REFERENCE EARTH MODEL (PREM) Solid Inner Core Liquid Outer Core Lower Mantle Upper mantle 0 1210 3480 5700 6371 Radius [km] Dziewonski and Anderson, 1981
P-wave travel time tomography Van der Hilst et al., 1998
S wave tomography SH SV
Seismic Anisotropy x = (Vsh/Vsv)2 Montagner, 2002
Motivation for seismic Q tomography: Faul and Jackson, 2005
3D Shear Velocity Models
“SH models” “SV models” Gung et al., 2003
S velocity Model: SAW24B16
AB CD Hawaii Q-1 “Pacific Superplume”
MN ST Q-1 Elastic SAW24B16 African “superplume”
ISOTROPIC VELOCITY RADIAL ANISOTROPY = (VSH/VSV)2 Panning and Romanowicz, 2004
African Superplume dlnVs ~ -3- -12% Wang and Wen, 2005 Ni and Wen, 2005
Vs Vf r Depth ~ 2800 km Ishii and Tromp, 2000
Data Model Anomalous splitting of core sensitive modes
Mantle mode Core mode
Hemispherical dependence of anisotropy (Tanaka and Hamaguchi, 1995)
Innermost Inner Core ? Ishii and Dziewonski, 2003
Fig. 1. Ray paths of PKP waves and example of waveform doublet used to detect temporal change of travel times through the inner core J. Zhang et al., Science 309, 1357 -1360 (2005) Published by AAAS
Fig. 1. Ray paths of PKP waves and example of waveform doublet used to detect temporal change of travel times through the inner core J. Zhang et al., Science 309, 1357 -1360 (2005) Published by AAAS
Fig. 4. Difference of BC - DF times, d(BC - DF), at station COL as a function of the time separation between the two events of the doublet J. Zhang et al., Science 309, 1357 -1360 (2005) Published by AAAS
STRONG MANTLE HETEROGENEITY? Map: enhanced tomographic map at The core-mantle boundary Bréger et al., EPSL, 2000
Current Challenges • Improving resolution of 3D structure: • Wave propagation in strongly heterogeneous 3D media/waveform inversion • Address uneven sampling (oceans) • Fine scale structure of major discontinuities • Attenuation tomography • 3D density structure • Combining information from seismology, mineral physics, geochemistry and geodynamics
Garnero, Ann. Rev. 2000 “Scenario for CMB”
Transverse isotropy dln x x = Vsh/Vsv 175 km 300 km