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9




            ,—
                 somemomemes
     Constraints
                                 Topography


               Levels
                 7)
     and
            Level
     Methods
                                                                  Observed

                                                                   Predicted
                              Drillhole
      Interpretation:
                                 {  ./
                                                                    swomeme
                                                                  ——
                                  C\
                                 Outcrop
                                                                   Gravity  Anomaly
                  Anomaly,
                ,
                Snavitnd
                  ravity
                                          Reflection.
                                 Surface
                                                   Inte rp. retation
            Constr aints
          :
                                          Seismic
                             50
                                                        +50
                +50
                     °
                                                             0
                    jepu
                                                             &
                                                                 s
                                                   b )
            a )
                  ;
                                                                                     Model       p=2,.82   je   Wy  nara   a   ?   p=2.39   p=2.48   p=2.51              include  1)  constraints   (Level   firm   a)  The  Constraints  and  interpreted  cross  section.   1.8  FIGURE   (Level  2)   firm   Less  the  drillhole.   in   and  the  surface  dips  observed  at  topography,  types  of  rocks,  and   from  profiles,  and  from  seismic  reflection  interpreted  orientations  of
                                example,   sur-  éxample,   geo-   of   models   other   the   Model   _        the surface.  Surface  outcrop   resulting  in   closer  to  eunane   not  changed.
             hand:              (for   sense   For   interpretations   suggest   in   predicted                      by  surface  geology  are
             your        observations.   levels.   further   Thinking   Predicted  from   —   Model
             in                 common                          Starting                                          testing  subsurface  densities  and  geometries,
             put   :   Earth.   direct   and   3)   (2,   constrain   region.   "Observed   Le                  at  several  stations  on   Densities  and  geometries  adjusted
             can   you   the   scattered   logic   lower   can   interpretations   in   the   Anomaly      cick ceed   constraints  offered
             that     about     on   to   (1)   1)              $0                              Model           measured   c)   the
             Earth      on  based   based   higher   (Level   geophysical   processes      b)             Observed   Predicted          Preliminary  model   that
             the      observations   observations.   region   or                           ——   rasme=   Adjusted   density  (g/cm?).
             of   samples.   interpretations   considerations,   from   flow   a   of   the   structure         Gravity  anomaly   =   anomalies.  Note
      Introduction   (Firm  Constraints):   atkervatioas   pe   Outcrop   cores.   Drill   Constraints):  (Softer   or  Indirect  inferred   Map   Geophysical  (Reasonable  Assumptions):   Theoretical   “modeling”).   should   mapping   2);  (Level   data   overall   for   Gravity  Anomaly                   §   #0   a)  Forward  modeling  example.   interpretation.  b)   (see  Chapter  8).  p   and  predicted
      Chapter   1   1:   Level   a)   b)   2:   Level   a)   b)   3:   Level   Thinking   face geological   physical   3)   (Level   es   and dips  serve  as  constraints  on  a  predicted  gravity  anomaly   between  observed
      8                                                                                                         1.7
                                                                  ydg  —=—                                      FIGURE   agreement

                                                                                             ;
      nn  eter            ee   ee
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