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زمینشناسی و معدن::
رانش صفحه
pattern demonstrates how the Pacific Plate drifted over the hot spot and during the Eocene at
caused a re-orientation of the plate drift pattern
magmatism to leave prominent and rather continu- ous tracks of plate drift in the ocean.
This re- orientation of the plate drift pattern in the Eocene caused the kink in the track.
The dashed red line tracks the position of the hot spot as reconstructed from the global plate drift pattern.
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