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A geodynamic model of mantle density heterogeneity

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Academic year: 2021

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Figure

Figure  1  shows tile  global lower  mantle  correlation be-  tween our  slabs and  SH425.2  as a  fimction  of  the  velocity  decrease at  670-kin  depth
Fig.  2.  Degree-by-degree correlations for  degrees 1  to  5,  over  the  lower mantle  between the  slab density model and  SH425.2
Fig.  4.  Density  heterogeneity  spectra  as  a  function  of  depth  deduced from  tomography  and  from  the  slab  model
Fig. 6. Stone  as in Figure  5 but at the depth  of 1000  kin. The level  lines  in Figures  61)  and  6c are 2.0 kg m -3
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