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

2005ES000179-fig01.html
Figure 1. Structure of mantle convection calculated at the stage of the aggregation of continents into a supercontinent. The dimensionless superadiabatic temperature is shown in color. The arrows are mantle flow velocities. The longest arrow corresponds to a velocity of 4 cm yr-1.

RJES

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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