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                                                information   which   in   within   the   force   of   magnetic   8.1).   (Fig.   ~   Leese,  ae  ~.,  K  ee  tae,  ~   i




                                                provide   those   are   of  observation   from  distance   simple.  Lines   while   poles   Field   Go   -  soit   Ls   IL   ~~,  —  Wy  Zen   (arrows)  have  a proximately  of  the  magnetic  field  is  governed  by  sche  fou)
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                                                that   fields   fields   position   with   is   field   Earth,   the   negative   and   b) Magnetic   \s   SK   XS  NX  \  \   .  \\   ed   eet.  sy   Looe  .   7               OS     /   :   -"   /


                        Isostasy   J.  the force  of attraction   Earth's   Gr.  stasis,  standing).  a   n.,  he  sutdy  of spatial   potential   are   Potential  Earth.   the   on  depend   field  decreases   Earth’s  gravity   of  center   positive  Earth’s   per   :   ee,   oo  PO  as   -   -   -   7   yw   4   “   ’   N\  “Semen  Pig.   ieee   incense   is  symmetric.  Force  vectors  factor  of  two  from  equator  to  pole.






                 8            L.  gravis,  heavy),   <  Gr.isos,  equal;  state  of balance  whereby  columns  of material  exezt  equal pressure  at   1 sii  sta’  st)   and  Earth's  gravitational field  and  their  relationship  to  the   Earth,   forces   the  within   field   the   potential   field,   toward   the   on  depend   fiel   y  gravity  field  magnitude  and  direction
                 Av PP BecR. «9  GH   and  Gravity   gravity  (grav'   |<   até)  n.,  between  masses  2.  the  force  that  tends  to  draw  beedies  in  sphere  toward  Earth's  center.   [<  ‘isostasy  (i sii  sta‘  sé)  n.,   and  below  a  compensating  depth.  gravity  and  isostasy  (grav'   até   variations  in  distribution  of  mass  within  the   gravity  Earth’s  magnetic   and   nature  materials   of   strength   of  direction   and   a   of  strength   the   magnetic









                                                                   Gravity
                                                      field:
                                                  the
                                                                   a)
                                                                                                    FIGURE   8.1   toward  and  point   negative














              A   and   Lillie,   the   (3rd.   pp.   and   and   A.   The   Oxford
              1989,   region  of   R.   beneath   analysis,   Dynamic   P.  Bailey,   tecton-   Geophysical   D.   and   Cambridge:   1997.
              BabuSka,   Geophysics   and   time   The   Geology   Sons,  Inc..  567   earthquake   of   earthquakes  mid-ocean  ridges, Journal   Sheriff.   Allen.   York:


              V.   thickness  in  the   of   Dobrath,   lithosphere   delay   115,  pp.  381-390.   1995,   Physical   R.  Pelton,  and  J.  Hotspot:  Contemporary   from   of   E.   Geophysics,   Press.  860  pp.   R.   New
              and   Studies   M.   seismic   Porter,   to   Journal   Mechanism   the  of  Geophysical  Research,  v.72,  pp.  2131-2153.   R.   C.   and
              Plomerova,   lithosphere   11-21.   Babuska,   the   of   from   C.   S.   Introduction  ed.).  New  York:  John  Wiley  and   B.,  R.  T.  Shuey,  Jr,   properties   data,  Research,  v.  82,  pp.  3665-3676.   Geldart,   P.   Applied   University   Sich,   Earthquakes,   Press,  568  pp.



              J.   of  the   Carpathians,   Structure   Rift  Geophysical  Journal,  v.   and   J..   crustal   1967,   nature  of  faulting  on   L.   M.,   1976.   K.   of
              P.,   Geodesy.  v.33,  pp.   Plomerova,  J.,  V.   Cameroon   B.   Earth:  An   R.   1977,  Yellowstone   and   acromagnetic   R.,   L.   W.   Cambridge   S..   R.   Geology   University
              PajduSak,   model   the   1993,   Skinner,   Smith.   ics   Sykes,   Telford,   Keys,   Yeats,



          Seismology   in  variations   of  epi-  location   of  America,   1984,  Hager.   beneath  structure   Letters,   Seismology   of  Journal   Cambridge:   V.   J.   and   (3rd.  Acoustics   York,   New   Sons.   Global  Modern   Series  Geophysics   pp.  Press.  52]   Plomerova.   J.   the   in  lithosphere  Carpathian-Pannonian   the   of  Tectonics   scismicity.   focal   80.   y.  Bulletin,



          Earthquake   Regional   1962,   the   on  Seismological  Society   B.  H.   image  of  mantle  California,  Geophysical  Research   1968,  R.  Sykes,   tectonics,   ed.).   (6th  Earth   Press.   Coppens.   B.   A.   of  Fundamentals   and  Wiley   1995,   and  BabuSka.   the   of  region.  Tectonophysics.  v.  23  pp.  215-235.   1969,   Sykes.   from   regions   America   of





          7   E.,  and  J.  Taggart,   their  effect   R.  W.  Clayton,  and   L.  Oliver,  and   global   new  Geophysical  Research,  v.73.  pp.  5855-5899.   The   1976.   University   Frey.   R.   A.   1982,   John   York:   Wallace,   C.   T.   International  Number  58,  New  York:  Academic   Bielik,  V.   modeling   Alpine-Western   R.   L.   America   Society
          Chapter   velocity  and   Bulletin   1037.   E..   tomographic   southern   v.11,  pp.  625-627.   the   H..   Cambridge   E..   L.   Sanders,   New   and   Seismology.   M.   J.,   R.   Gravity   Eastern   and   P..   Middle   Geological   1639-1684.


           222   Herrin,   Pn   centers.   v.52.  p.   Humphreys,   A   Isaacs,  B.,  J.   and   Jeffreys.   Kinsler,   ed.),   480  pp.   T..   Lay,   Lillie,   1994,   Basin   Molnar,   pp.
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