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

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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