Page 361 - Whole Earth Geophysics An Introductory Textbook For Geologists And Geophysicists
P. 361

343

         Text
         in
         Used                              Nm?/kg?)
         Abbreviations                     107!!   (3.1416)



                                           X   of  circle   field   field   gravity         z
                 plate   plate             (6.67      magnetic   field   magnetic   field   in   gravity   x   to   to

                 elastic   elastic         Constant   diameter   magnetic   horizontal   magnetic   of  change   in   respect   respect   x   to

                 above   below               to       horizontal   of   of   of   field   field   field   of  change   of T,  with   with   of  T,   respect

                  material   asthenosphere   mantle   susceptibility   Gravitational   of  circumference   field   of   component   component   magnetic   magnetic   magnetization   magnetization   gravity   component   component   to   Ag,,  with   operator
                air   of  material   of  crust   of  water   (degrees)   ratio   magnetic   component   component   ambient   magnetization   derivative   derivative   of
                of   of   of   of                                         in       Symbols   proportional   in   convolution
              density   density   density   density   density   density   density   density   period   latitude   Poisson’s   magnetic   Universal   ratio   total   east   horizontal   north   vertical   Earth's   induced   remanent   total   induced   remanent   change   horizontal   vertical   change   first   partial   integral


                                        Constants   Vectors
                                                              £
                                                                2
                                                                        —
                                                                         100  16D  16D
                                                                      z
                                                                        =
                Ps   Pz   Pa   éc¢ddpwoe  x   G   v   Sf   the   E   ry   Fy   Fy   bea  5  =  é  1  >  <1  <1  <1   Mathematical   as   A   dT/dX   éT/az  dx   Ag,   J   *






















            downdip   updip   layer   n   B   n                                     determination

        Abbreviations   shooting   shooting   i"   the   Jayer   at  receiver   along   Jayer   wave   ;   magnitude   (degrees)   gravity   gravity




        and   when   when   within   time   along  refraction   shot   A,   at   wave   refraction   wave   refracted   n   earthquake   distance   gravity   in  change   in  change
        Conversions,   intercept   intercept   travel   for   time:   direct   wave   reflected   critical   time   of  compressional   critically   wave  of  shear   layer   of  i"   layer   of   velocity   wave   velocity   plate   for   angle   epicentral   anomaly   anomaly   of  change   in   of  horizontal   of  vertical   gradient




        Units,   T-axis   refraction  T-axis   two-way   intercept   time   travel   correction   of   time   of   time   time   for   moveout   time   of   time   time   displacement   velocity   velocity   velocily   velocity   velocity   velocity   square   velocity   wave   velocity   of  elastic   distance   distance   distance   distance   of  interface   factor   declination   gravity   gravity   angle   of  incidence   of  refraction   constant   modulus

        —   refraction   vertical,   T-axis   travel   refraction   terrain   travel   travel   travel   normal   arrival   travel   arrival   fault   initial   volume   velocity   apparent   average   seismic   interval   seismic   compressional   mean   shear   deflection   width   horizontal   critical   crossover   vertical   angle   correction   magnetic   earthquake   Bouguer   air   magnitude   magnitude   magnitude   geothermal   critical   wavelength   Lame’s
        AppendixB   to-a                                     root   true         dip       free    dT /az   angle   angle   angle   shear




        342   hie   q   i   T                                                                     Ag,   ceoonK  «K  2
   356   357   358   359   360   361   362   363   364   365   366