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Is inner core translation a good model ?. Vernon Cormier, Lizzie Day, Zack Geballe, Marine Lasbleis , Mohammad Youssof , Han Yue. Does the inner core grows layer by layer?. Does it convect ?. Deguen , 2012. Summary of s eismic features. SLOW isotropic velocity
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Is inner core translation a good model? Vernon Cormier, Lizzie Day, Zack Geballe, Marine Lasbleis, Mohammad Youssof, Han Yue
Does the inner core grows layer by layer? Does it convect? Deguen, 2012
Summary of seismic features • SLOW isotropic velocity • Less attenuation (high Q) • More anisotropic • FAST isotropic velocity • More attenuating (low Q) • Less anisotropic West East Inner inner core? Modified from a figure by Jessica Irving
Hemispheres of P-wave travel time Waszek & Deuss, JGR, 2012
Composition is an unlikely cause < 8.8 mol % Si 8.5 mol % Si Cottaar and Buffet (2012) Alfe et al. (2002)
Translation: a type of convection Slow Fast Monnereau et al., Science, 2010
Age distribution in a translatinginnercore 0 km 100 km Age (Ma) 500 km 300 km 0 75 150
Tuned parameter #2: Domains grow to ~ λseismic/2π Calvet and Margerin, 2008
Other seismic features West East Inner inner core? Modified from a figure by Jessica Irving
Future tests • Try to explain innermost inner core with a textured polycrystalline scattering model • Test a spectrum of iron elasticity models • Map Vp in different frequency bins • Map Q Conclusion: Rigid translation is consistent with observed hemispherical variation in Vp provided that: domains grow to approximately λSeismic/2π , the iron alloy making up the inner core has relatively high elastic anisotropy