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3D seismic imaging of the earth’s mantle Barbara Romanowicz Department of Earth and Planetary Science U.C. Berkeley
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Surface waves
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P P S SS Surface waves Loma Prieta (CA) 1989 M 7 earthquake observed at KEV, Finland
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Shearer, 1991 Global Transverse Component Stacks
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After Park et al, 2005
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Sumatra 12/26/04 M9.3 (0.8 to 2.2 mHz) CAN UNM 0S7 0S9 3S2 0S6 1S4 0S11 1S5 1S3 /3S1 0S8 0S5 0S0 200 hours starting 10 hours before origin time 0S10 0S12 mHz x10 0S5 0S13
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PRELIMINARY REFERENCE EARTH MODEL (PREM) Dziewonski and Anderson, 1981 Radius [km] Solid Inner Core Liquid Outer Core Lower Mantle Upper mantle 637112103480 0 5700
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( Albarède and van der Hilst, 1999
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Van der Hilst et al., 1998 P-wave travel time tomography
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SH SV S wave tomography
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Montagner, 2002 = (Vsh/Vsv) 2 Seismic Anisotropy
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Motivation for seismic Q tomography: Faul and Jackson, 2005
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3D Shear Velocity Models
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“SH models” “SV models” Gung et al., 2003
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S velocity Model: SAW24B16
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ABCD “ Pacific Superplume” Q -1 Hawaii
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MNST African “superplume” Elastic SAW24B16 Q -1
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Panning and Romanowicz, 2004 ISOTROPIC VELOCITY RADIAL ANISOTROPY = (V SH /V SV ) 2
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Wang and Wen, 2005 dlnVs ~ -3- -12% Ni and Wen, 2005 African Superplume
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Vs VV Ishii and Tromp, 2000 Depth ~ 2800 km
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Garnero, 1998
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Courtillot et al., 2003
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The Earth’s inner core
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Anomalous splitting of core sensitive modes Data Model
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Mantle mode Core mode
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(Tanaka and Hamaguchi, 1995) Hemispherical dependence of anisotropy
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Garcia and Souriau, 2002
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Innermost Inner Core ? Ishii and Dziewonski, 2003
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Differential rotation of the Inner Core
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Published by AAAS J. Zhang et al., Science 309, 1357 -1360 (2005) Fig. 1. Ray paths of PKP waves and example of waveform doublet used to detect temporal change of travel times through the inner core
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Published by AAAS J. Zhang et al., Science 309, 1357 -1360 (2005) Fig. 1. Ray paths of PKP waves and example of waveform doublet used to detect temporal change of travel times through the inner core
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Published by AAAS J. Zhang et al., Science 309, 1357 -1360 (2005) 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
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Bréger et al., EPSL, 2000 Map: enhanced tomographic map at The core-mantle boundary STRONG MANTLE HETEROGENEITY?
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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
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Cartoon from Cazenave, 2002
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Garnero, Ann. Rev. 2000 “Scenario for CMB”
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Cartoon from Hellfrich and Wood, 2001
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“SH models” “SV models”
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Fukao et al., 2001
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175 km 300 km Transverse isotropy dln = Vsh/Vsv
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- 0 - 100 - 200 - 300 - 400 km
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Upper mantle:Q - lower mantle: Vsh Degree 2 only
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QRLW8 Hotspot distribution Weighted by buoyancy flux Attenuation tomography
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Anelastic attenuation: QRLW8 Gung and Romanowicz, 2002
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