|
|
|
|
|
|
|
|
|
- influence of
the major up- and down-wellings
|
|
|
get less
|
|
|
- more drop like
instabilities
|
|
|
- still a large
scale cirulation (shear flow)
|
|
|
=> looking at
the Earth mantle with Ra > 10**6
|
|
it seems impossible to preserve
chemical
|
|
|
|
heterogeneities
over a long period of time
|
|
|
=> Earth
mantle must have lateral distincted
|
|
|
|
reservoirs
|
|