Page 196 - Whole Earth Geophysics An Introductory Textbook For Geologists And Geophysicists
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                      TIBETAN
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                        CRUST
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                                                                                                                          6.39  FIGURE  a) Cross section  showing  position  of  INDEPTH  seismic  reflection  profile,  relative  to  model  of  underthrusting  Indian  continental  crust.  b)  INDEPTH  profile  in  southern  Tibet.  The  MHT  is  the  Main   the   from  to  be  the  décollement  separating  the  underthrusting  Indian  craton  Himalayan  Thrust,  believed  overriding  Hi
        Profiles   Hinterland———=>   South                             (Schweizerische  Arbeitsgruppe   the  toward   becomes  involved   in  Piffner.  W.  Frei.  P.  Valased,  M.   permission   (a).   the   and   beneath   the   and   (Figs.  6.18-6.20).   portions   1981;   1979,   6.39).   continental   6.36a).   (Fig.   indi-   may   Makovsky
        Reflection                                                       rises  southward   basement   Redrawn  with   1990.   1990),   al.   et   image   to   crust   the   beneath   al.,   et   Fig.   1993;   normal   partially   that  reflections   6.36b;
        Seismic   TT                                                   Switzerland   It  section.   crystalline   O.   (Pfiffner   difficult   is   of  thickness   structure   depths   (Cook   al.,   twice   melt   (Fig.  levels
        Of       Paes                                                  eastern   side  of  the   the   depth.  From   1327-1355,  ©   ..   boundary   from  Moho   Appalachians   (Zhao,  et   nearly   to   strong
       interpretation   5km                                              north   the   that  reveals   10  km  to  about   vol.  9,  pp.  Union,  Washington,  D.C.  Box  shows  approximate  position  of  seismic  profile  in   the  Alps  1983),   1986).   great   the   of   complex  beneath   reflections   the   Himalayas   becomes   enough   hot   reveal  Plateau   mid-crustal   at
       Tectonic   :   Serer                                            limb  of  Aar  Massif  in   2.8  s  on   is  at   traverse   Basin   Tectonics,   al.,   et   Smythe,   and   crust/mantle   because   reveal   including   the   and   crust   the   become   the  Tibetan   material
       And                                                Heivetic  nappes   of  longer  reflection   Molasse   the   S.  Smithson,   (Ando   (Beamish   The   ranges,   reflectors   ranges,   Alps,   Where   may   molten
       Structural   geome                                               profile  across  northern   top  of  basement   from   Appalachians   Reflections   mountain   -   resolving  profiles,  nonetheless,   mountain   1985),  the   Melt   rocks   from  profiles   of
       6     Foreland                                                      massif.  b)  Interpretation   extends  southward   Caledonides   8.Moho   collisional   al.,   et   Partial   granitic   ponding   1996).
       Chapter                                                         Reflection   a)  Reflexionsseismik,  1988).  The   it  Stauble,  L.  Levato,  L.  DuBois,  S.  Schmid,  and   Geophysical   northern   British   collisional   oblems  of   pr   Seismic   of   Nelson   9.   thickness,   Reflection   the   cate   al.,   et
       178   <==   North   O  -pe   ™   N                              6.38   center  of  the   thrusting  when   of  the  American
             a      (s)  euny  Jaaesy  ABA-OML   9                     FIGURE   fiir
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