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269

       Expressions
                           Weveunete
       Gravity
       their
                           ~__ tong
       and
       Settings
                           Free‘Air Anomaly
       Tectonic
                           100 -
    Se  eae  ee
                        3  km
                          (Moho
           Contributions  of three  Gravity  Observed  fundamental  boundaries  and  resulting      ridge  local  isostatic  equilibrium.  The  depth  Bouguer Anomaly  180  km.  Model   emg  KONE  “ay  SUagatese  18.0  km   =   Ree      km.   157.0   (Moho  depth   km)   12.5   =   than  is  more   has  thin   region   the  to  the  standard,  continental  (Figs.  8.40,  8.41;  compare   the   to   margin  passive     200      Likewise,  the   has  background  -2000   —300  mGal.   R
                        =
                                thickness  of  asthenosphere
                             thickness  of  mantle  part  of
                        thickness  of  water  column
                          km
                          2
                         =
                           5km)
           8.45   gravity  anomalies for  a  mid-ocean   is  of  compensation   parameters  are:   thickness  of  crust   =   depth   lithosphere   =  column  Away from  the  ridge  (pormal  oceanic   =Skm   km   7.5   km   167.5   Moho  contribution  +300  mGal,  because   portion  of  the   model,  Fig.  8.44).  bathymetric  contribution   than   elevated   and   and   the   flanking   the   associated   with   Figs.   in   due  ridge,   observed   topographic   anomalies   those
           FIGURE   in   On  the  ridge:   =   h,,   =   h,   =   h,,   =   hy   lithosphere):   h,   =   h,   =   h,,   =0.   h,   The       crust,  relative   craton   seaward   values  less   of  the   ridge   Moho   the   from   of  effect   deep   with   high   a   contribution,   level   continental  margin   over   the   anomalies   the  mimic   lows   longer  wavelength   with  agreement
                                                          Bee                           weight   the  supports   ridge   the  across   from  resulting   the   displays   thus   bathymetric   the   300  Gal  background   passive   the   values  anomaly   gravity  Bouguer   highs   and   The  uncompensated.   general   in
       lsostasy                                 -300                                        low   anomaly   removing   for   Bouguer   and   Short-wavelength   are
       and                         4  ee                                                asthenosphere   gravity   in   broad   gravity   than   more   anomaly   in   air   free   is   that
       Gravity                                                                            changes   on   a   air   effectively   the   drop   shows   Ridge.   which   amplitudes

           +500                                        0                                      free   shows   Bouguer   a   is   asthenosphere.   floor,

       8                                                                                the elevated   resulting   8.46   sea   and
       Chapter                                                                            The Positive   superimposed   The   After   anomaly   crust   (see   8.44).  There   vated   Fig.   :   Mid-Atlantic   the   widths
                Contributions   ==   ——   sruese   =———m
                                        Bouguer
       268        Moho   Bathymety   Gravity Anomalies  jepuw  Free  Air   Mid-Ocean   Ridge   of             on
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