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            velocities  for  the  models  in   be   might  how  they   of  error.  sources   recorded  profile  single  dipping  interface  model,  interpret   dip  interface;  b)   the   B.   and   2.0   changing   of  section   the   for  P-wave velocities   thicknesses  crustal   the   N   47°   along  section   (a).   in  illustrated   Geological   172,  pp.  103-128.   Geophysical   to  Introduction   McGraw-Hill,   York:   New   San   from  structure   from  Nevada,  Eureka,









            and  actual  differences  and   possible   refraction  reversed   below   and   below  points  A       L—   cross   a   draw   add   for  reasons   cross   a  draw   you   and  W.  D.  Mooney,  Boulder,  Colorado:  Society  of America,  Memoir   1976,   ed.),   (3rd   Crustal  1963,   to  California,  Geophysical  Research,  pp.  5789-5806.   Crustal   from  California   Northern   of   of  Mines  Division   The  basin,  Quarterly  Journal  of the  Royal Astronomical
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        Refraction   how  differences  in  Exercise  4-3  might  be  due   below   graph   at  A,  then   true   a)   depths   é   a   North   of   map   N   40°   your   to   central   reasons   Sierra   1967,   158,  pp.  1407-1417.   seismic   deep   and   Geology   Academy   Slovak   the   of   (2nd  Evolution   Pub.  Co.,  403  pp.   geophysics   Cliffs,   P.  Riddihough,  1989,  The  crustal   continental   C.   L.   by   edited


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        98                                                                            Bateman,   Berdnek,   Bott,   Burger,
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