RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 7, ES3001, doi:10.2205/2005ES000179, 2005


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Animation 2. The animation shows the structure that arose by the time moment t = 340 Myr and is hypothetically conceivable as a future Atlantic Ocean when its greatly extended oceanic lithospheric plates will start sinking at the margins of Europe and North America. From this time, the Atlantic Ocean can be similar to the present Pacific Ocean.


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Citation: Trubitsyn, V. P., and A. P. Trubitsyn (2005), Evolution of mantle plumes and uplift of continents during the Pangea breakup, Russ. J. Earth Sci., 7, ES3001, doi:10.2205/2005ES000179.

Copyright 2005 by the Russian Journal of Earth Sciences

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