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faults  offsetting,   Province,  24, 25   for,  264-65,   maps  for,  272   (table),  322   interpretation   162  (figure),   anomaly,  259  (figure).  260   waves;  Shear   196,  206,   190,   for,  53,  54   tectonic  model,  270   rift  zones,  264,  265   (figure),  234   ridges,  268-69   ranges,  259,  274   margins,   isostatic   (figure),  234   148   146,   353




                               normal   magnetic,  296,  297,  299  (figure)   177   Range  (figure),  26  (figure),  28  (figure),  90,  92.  96  (figure)   gravity  anomalies   gravity  anomaly   in,  321  (figure),  323  (figure),  324   (figure),  325   reflection   161   160,   Island,  286  (figure)  Bathymetry,  260,  262,  263,  268   178   175   Uplift,   volcanism,  34   177   waves,  See  also   Compressional   earthquakes  and,   propagation  of,  47   travel-time  curves

                               flexural   169-71   structures,   Basin  and   266   flow   heat   seismic   159,   in,   Bathhurst   Batman   (figure).   Beamish,  D.,   Benton   Bimodal   Ridge,   Blue   Body   waves   207   260   complete,  232   in  composite   at  continental   equations   on   mid-ocean   at   mountain   at   at   for  regions   simple,  230-31   Bow   (figure),   Braile,  L.  W.,  92   Isles,   British




                               Mountains,  29,  92,   178,  322  (figure)   velocity,  68,  75  “earthquakes  and,  206,  208   inter-  horizontal   ‘from  single  dipping  interface,   177  (figure)   19,215.  See   16,   15,  Lithosphere/asthenos-   boundary  continental  rift  zones  and,  24,  325   (figure)   17   187,201,   186,   seismic  refraction  and,  37   164  (figure),   Control  (AGC),   198  planes,   113-16  dipolar  model,  285,  288  magma  chamber  (AMC),   175





                               Appalachian   177,   Apparent   (figure)   from  several   faces,  79   88-89   Argon,  302   Basin,  Arkoma   Asthenosphere,   also   phere   14  defined,   description  of,   earthquakes  and,   205   gravity  and,  38   properties of,  217   seismic  waves  and,  46  volcanism  and,  31,  32,34   Adlantic  Ocean,  95   (figure)   Attenuation,  4   Automatic  Gain   113   fault  Auxiliary   Average  velocity,   Axial   Axial   162-63   Bachmann,  G.






                                  178  (figure)   wedges,  26  (figure),   chaotic  expression  of  deformed   171   147-50   171   169,   168,   159,  rift  zones,   171  basin  sediments,   and,  64   122-24   102  reflection  and,   118,  Acquisition.  See  Seismic  acquisition   (figure)  315, 316, 317   model,  255,  260-61,  262,  272   ranges,  256,  259,   159   177,   175,  (figure),   for,  269-70,   gravity  anomaly  maps  for,  272   (table)   161   160,   (table),  345,

               Index            A   177,  Aar  Massif,  Absolute  gravity,  234,  235,  236   113  Absorption,  Acceleration.  See  Gravitational   acceleration   Accretionary   146   27,37,   sediments,  earthquakes  and,  205   Nankai  Trough,   in  in  subduction  zones,  Acoustic  impedance,  4,  57   in  continental   161-62   forearc   in   reflected  arrival  reflection  coefficient  and,   seismic  seismic  waveforms  and,   122-24   Advection,  Aeromagnetic  surveys,  296













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               level)   level)   km
               below  sea   below  sea   40.6   =   z   km   1   =



        Exercises   +26.4  mGal   boundary  47.5
     :         km   — 138.3  mGal   km   —234.6  mGal;   +234.6  mGal;z

        Selected   =   =   (Moho  46.2   =   =


        to   Ag(Moho)   (lith/asth   Ag(lith/asth)   km   Ag(Moho)   Ag(topo)   °C/km
        Answers   Maximum   km   Maximum   11.2   =   Maximum   Maximum   29.7   0.08  W/m?   =35km   ~60km   ~20km   ~=35km




        D   ii)   82.5   =   hy   i)   -   Az(Moho)   i)   ii)   ~6cm/year   cm/year   4.7   =   dT/dz   q   ~   =  i)   ii)   i)   ii)
        Appendix   b)   c)   a)   8-8   b)   b)   9-4   =   9-5   a)   10-1   b)   a)   10-3   b)



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