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at   focal   the  same
             view  of  radiation   San  Andreas  boundary  (Fig.  2.20).   for   (a),  plotted   Auxiliary  fault   first-motion   have   Foca)   the   pattern   the   lower   the   dilatation   by   from   fault   mechanism   for   boundaries.   material   .   (Fig.  7.3b)
         199        arrival   as  a   resulted   is  exactly  the   right-   fault   solu-   the   the   and   the   nor-   (up

         Tectonics   Map   a)  for  right-lateral,  strike-slip  fault   information   in   solution.  c)   of  the   (a),  showing  that   pattern  could   lefi-lateral  fault.  d)   (c)   for  solution   from  resulting   (a).   on  reverse)   of   view   mechanism   of   7.17b).   encompassed   degrees)   the   of   indicates   focal   faults,   plate   brittle   transform   to  moderate  magnitude



         Plate   7.15   occurring  along  the   plate   First-motion   indicated   interpretation   information  in   in   fault   compression/dilatation   or   a   focal   regions   (Fig.   (in   dip   of   diagram   of   auxiliary   with   cold,   and  lithosphere  remains  shallow  (Figs.  2.11;  2.22).
         and   FIGURE   pattern   transform   b)   stations   mechanism   radiation   from  a   mechanism   same  as  that   lateral   ~   (normal   faults depict   The   by   fault   angle   the   distances   angles   the   of   examples   and   associated   relatively   2.7, 2.8,  7.3).   (Fig.  7.3a)
         Earthquakes             Compression   Dilatation           a  make   movement   dip-slip   7.16c).   (Fig.   surrounded   normal   a   1)   that:   the   2)   the  indicate   portion   inside   shows   7.19   earthquake   is   of  configuration   (Figs.   divergent





                                 Black  =   White  =                surface   the   of   sense   for  solutions   see  would   compression   represents   7.18  illustrates   90°;   equals   diagram   the   of   Fig.  plane.   the   of   TECTONICS   activity   the   lithosphere   Boundaries   at  boundaries  earthquakes  are  typically  of small

                                                                    on   and   bird   a   has   pattern   of  the   trend   sections   faults.   PLATE   seismic   reveal   of  the   Plate   earthquakes  occur   brittle  part  of  the
                                                                    stations   angle   mechanism   that   fault   projections,  Fig.   diagram   portion   the   3)   fault   cross   strike-slip   most   part


                                                                    at   dip   opposite   the   and   earthquake   with   AND   that   depths   upper   Transform
                                                                    arrivals   to   Focal   the   such   planes;   along   shows   the   shallow  focus  boundaries,  because  the
                                                            .  4  .  A  .  ee,   the   reverse   of   inside   and   focal
                                                                    First   relates   for   For   inside   to  edges   ‘auxiliary   of  strike   solutions,   EARTHQUAKES   7.20   Earthquake   comprising   Only
                                  ©                                     7.16b).  half  of  the  focal  sphere   a   7.17a);   portion   the   the   reverse,   and   divergent
                                  C=Compression   Dilatation   =   D   that   (Fig.   tion   (Fig.   mal,   Fig.   Divergent   At















             Initial ground  motions  and   Initial   the   pushes  up;  the  Z-component  shows  an   as  a   arrival   Initial  pulls  the  ground  down;  the   shows  a  downward   first   Me   Time  —=>   in   (a).   by   and   the   actual   have   focal   of   view   dip-slip   be   can   earth-








             7.13  Z-component  seismograms  for  P-wave  arriving  at  a  seismic  station.  (a)   compression   as  a   first  motion.  (b)   First  Motion   b   Down   7   First  Motion   Up   2   First  Motion   Down   3   a)  Waves  radiate  outward   synthesized   be   compression   determine   the   to   could   also   called   are   map   a   have   that   dilatation   the   of
             FIGURE   arrival   ground   upward   dilatation   Z-component   motion,    three  stations  highlighted  in   can   of   7.15b).   uniquely   perpendicular   fault)   dilatation   simply   and   section

                                                               fl                              quadrants   (Fig.   not   are   faults   cross
                                                           Woh     3            .   :   for  the   information   with   does   A   fault   strike-slip   and   they  faults,   For  7.15b,d).   of  compression   around   a


              First  Motion                              Ground   Moves   fj   latation   .  “\   \,  ‘s  earthquake  occurring  on  a  reverse  fault.   seismograms   first-motion   circle,   a   white,  respectively   7.15a   Fig.   in   earthquake.   left-lateral,   a   compression   strike-slip   (Fig.   quadrants   sphere)



         Seismology   S.                                   Up.   ff]        i   \   ON   Compression   Z-component   7.15a. The   stations   on   and   black   pattern   the  caused   case   this   in   quadrants   of   vertical,   stations   faults),   (focal   circle   7.16a).



         Earthquake                         --   ren     Ground   2  Moves   il         dilatation.  b)  The   Fig,  view  in   the   from   by   the  observed   that   7.15c).   (Fig.   depicting   For  solutions.   seismic   at   reverse   and   a  drawing   (Fig.   fault




                                             ene   5             “Co                  Initial  P-wave  radiation  pattern  from  an   map   arrivals   represented   that   fault   the  (auxiliary  fault  plane;   responsible   Diagrams   arrivals   (normal   by   and
         Chapter7                             “—~@=p-   Initial   Dilatation   Down   ™~  ff   and   on  shown   plotting   dilatation   Note   of  nature   one   been   mechanism   initial   motion   visualized   quake   focus




         198                                             Ground   Moves   a   fl   4   7.14  quadrants  of  compression   the
                                              Focus                                   FIGURE
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