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290   CHAPTER 10





                                                                            10˚N






                                                                               0˚




                                                                South American
                                                                     Plate
                                                                            10˚S

                                                                    Brazilian shield
                                 Nazca
                                  Plate
                                         Nazca Ridge                        20˚S











                                                                            30˚S








                                                                            40˚S
                               Chile Rise

                               90˚W                 75˚W                 60˚W

           Figure 10.2  Earthquake focal mechanism solutions in South America from the Harvard CMT catalogue for shallow

           (<70 km) earthquakes (1976–1999) (image provided by M.-A. Gutscher and modified from Gutscher et al., 2000, by
           permission of the American Geophysical Union. Copyright © 2000 American Geophysical Union). Shaded relief map is
           from data base of Smith & Sandwell (1997). Dark gray triangles are volcanoes.



           respond to the partially subducted Nazca Ridge and   tions that the subduction of thick, buoyant oceanic
           the fully subducted ridge beneath the Inca Plateau. A   lithosphere leads to flat subduction and can terminate

           lithospheric tear may occur at the northwestern edge   magmatism by eliminating the asthenospheric wedge
           of the flat slab. These relationships support interpreta-  (Section 9.6).
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