The finding of the team Matthew Agius can affect our models and reconstructions of Pangaea in the following ways:
By letting us believe instead of assuming that the force of gravity is the primary reason for the movement of tectonic plates, the movement of upwellings under the ocean could play a major role than initially thought.
There are possible occurrences that could make upwellings from about 700 kilometers deep move towards the Earth’s surface, improving our understanding of the Atlantic Ocean formation.
Matthew Agius's team's findings were revealed in a journal titled "A thin mantle transition zone under the equatorial Mid-Atlantic Ridge."
Hence, in this case, it is concluded that the finding of the team Matthew Agius can affect our models and reconstructions of Pangaea."
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