Shifting core may have accelerated land movements

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The discussion centers on the phenomenon of True Polar Wander and its implications for understanding continental drift. Recent analyses of magnetic signatures in ancient rocks provide stronger evidence for the rapid movement of continents across the equator approximately 700 million years ago. Critics argue that the methodology used to estimate the latitude of rock samples relies on circular reasoning, as it assumes the magnetic pole aligns with the geographic pole. This debate highlights the complexities in interpreting geological data and the assumptions underlying magnetic orientation studies.

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Ivan Seeking
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Seven hundred million years ago our planet experienced sudden contortions that sent whole continents flying across the equator in just a few million years. This idea has been controversial, but is now on a much firmer footing after a new analysis of magnetic signatures in ancient rocks. [continued]

http://www.nature.com/nsu/040517/040517-13.html
 
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Good catch Ivan Seeking.

There has been some controversy indeed about this phenomenon of the True Polar Wander.

The main objective, magnetic orientation, is however a circular reasoning.

Continental drift is derived from three dimensional magnetic orientation of rock core samples. This way the lattitude of the sample can be estimated, when it was formed with the prior assumption that the magnetic pole would also be the geographic pole.

Now if somebody assumes that the whole mantle- lithosphere wandered around, the magnetic orientation is used to "refute" it. So how does that work: the refuter -uses the calculated latitude of the samples (unaware of how it was calculated) to show the position of the magnetic North Pole assuming that this would be identical to the Geographic North pole. And of course things add up exactly.
So as a result he sees not a trace of a True Polar Wander. No wonder, since it's circular reason. A used to get B. B used to get A.

BTW The current magnetic Soutph Pole is not even within the southern (ant)Arctic circle.
 

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