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SUBDUCTION ZONES  281





                                                                   2000m bathymetric contour
                                                                   Trench
                                                                   Active spreading center
                       10  S
                                                                                 Samoa
                                       Coral
                                       Sea                   Vanuatu
                                       Basin
                                                     New             Fiji
                       20  S                       Caledonia


                                                                   South    Lau Ridge Lau Basin
                                                       New          Fiji      Kermadec Ridge
                                                     Caledonia     Basin
                             Australia                 Basin                   Kermadec-Tonga Trench
                                                                 Three
                       30  S                                     Kings
                                                     Lord        Rise
                                                    Howe              Havre
                                                                      Havre
                                                     Rise             Trough
                                                                      Trough
                                            Tasman
                                              Sea
                                                               New
                       40  S                                 Zealand          Taupo
                                                                           Volcanic Zone
                                                                         Chatham
                                                                          Rise
                              0        1000       2000

                       50  S            km                     Campbell
                                                                Plateau
                           140  E      150  E      160  E      170  E      180  E
            Figure 9.31  Map showing the location of backarc basins in a part of the southwest Pacific, including the Lau basin,


            the South Fiji basin, the New Caledonian basin, and the Taupo volcanic zone (modified from Collins, 2002b, by
            permission of the American Geophysical Union. Copyright © 2002 American Geophysical Union). Box shows location of
            Fig. 9.32.



            magma addition and the age of the crust. In the Mariana   Structures corresponding to a mid-ocean ridge are
            Trough (Fig. 9.1), for example, crustal thicknesses range   not always present in backarc basins, and magnetic
            from 3.4 to 6.9 km, with the thinnest values correspond-  lineations may be poorly developed (Weissel, 1981).
            ing to either slow spreading centers or magma-starved   Those lineations that are present can be correlated with
            regions, and the thickest crust corresponding to regions   the magnetic polarity timescale (Section 4.1.6), although
            of high magmatic activity (Kitada et al., 2006).  they tend to be shorter, of lower amplitude and less
               These observations and the evidence for extension   clearly defined than oceanic anomalies. In the southern

            and sea floor spreading imply that backarc crust in   Lau Basin, for example, individual magnetic anomaly

            oceanic settings is generated in a manner similar to that   lineations cannot be traced for more than 30 km along
            occurring at mid-ocean ridges (Section 6.10). However,   the strike of the basin (Fujiwara et al., 2001). This short

            there are many important differences in the processes   length probably reflects the small size of basement
            that form basaltic crust in these two environments.   faults, which typically display segmented, en echelon
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