fig12.htm

Figure 12. Residual gravity anomalies (in mGal) obtained after the following fields were subtracted from the Bouguer anomalies: the gravity field of the sedimentary cover, anomalies due to Moho depth variations, and regional fields produced by the most significant masses located outside the calculating area up to the antipodes (see the text). The solid crust density is constant and equal to 2.84 g/cm 3.


This document was generated by TeXWeb (Win32, v.1.3) on August 28, 2000.