RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES4001, doi:10.2205/2007ES000218, 2008

Figure 6. (a) Isostatic anomalies calculated by authors from Bouguer anomaly and from relief
(ETOPO5, 1993) for average crustal density for ocean (of 2.8 g cm-3) and that for continent
(of 2.67 g cm-3), and that for mantle (of 3.3 g cm-3),
respectively integrated at 166 km radius by
Airy model and surface reduction depth of 33 km. Long-wave components of above 900 km were
removed from anomalous field.
(b) Isostatic anomalies calculated by authors from Bouguer anomaly and from relief
(ETOPO5, 1993) for average crustal density for ocean (of 2.8 g cm-3) and that for continent
(of 2.67 g cm-3), and that for mantle (of 3.3 g cm-3), respectively
integrated at 166 km radius by Airy model and surface reduction depth of 33 km. Long-wave components
of above 900 km were removed from anomalous field.

Citation: Sokolov, S. Yu., N. S. Sokolov, and L. V. Dmitriev (2008), Geodynamic zonation of the Atlantic Ocean lithosphere: Application of cluster analysis procedure and zoning inferred from geophysical data, Russ. J. Earth Sci., 10, ES4001, doi:10.2205/2007ES000218.
Copyright 2008 by the Russian Journal of Earth Sciences
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