Page 352 - Whole Earth Geophysics An Introductory Textbook For Geologists And Geophysicists
P. 352

of
                                                  ideas
                                   topo-
                                                DISCUS-
         335
                                                                                 mantle.
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         Paper
                                                                                 upper
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                                                  interpretations
                                                the
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         Components
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                                       lithospheric
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                                                       long.
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                              mountain
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                                                  own
                                                heat  flow.
                                                                                 within
                                                       10  pages
                                   of
                                                                        beneath
                                                  student’s
                                   weight
                                                     the
                                                                                         oceanic
                                                                      of
                                     mid-ocean
                                             course
                                       isostasy,  suggesting
                                at
                              of
                                                                                    observations/interpretations:
                                                     of
                                                                                 transitions
                           new  observations/interpretations:
                                                                      orientation
                                deepens
                              topography
                                                       to
                                                     evolution
                                                and/or
                      changes;
                                   supporting
                                                       &
                                                                        basement
                                                                                         vs.
                        region.
                                                                          reversals.
                                             of
                                                  the
                                                       now
                                                          available:
                                                                                         of  continental
                                                            above).
                    changes;
                                     and
                                             12%
                                water
                                                  of
                                                magnetics
                                                                                 brittle/ductile
                                                       is
                                                                      Susceptibility.  size,  and
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                        the
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                                                       Body
                                     rifts
                  distribution;
                                                               above).
             above).
                              high
                                                                        crystalline
                                                                          magnetic
                                             week;
                                   asthenosphere
                                                            (see
                        of
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                    thickness
                                     continental
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                                                       Main
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                                                     and
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                  Density
                                                               Earthquake
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                                                Revise
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                                                                                                                         ridges?  mid-ocean   at  created  of  seafloor   Age   ¢   deposits?  sedimentary  of  continental   Age   ¢   formed?   they   as  of  rocks  Latitudes   e   Flow:   Heat   lithosphere?   of  the  Thickness   ¢   sources?  magma   to  Proximity   ¢
        Course   the   of   double   Main   The   continental   ridge?   infor-   3   now   stress?   range?   now   Body
        Geophysics   structure   typed.   be   Figures.   a   at   mid-ocean   adding   and   Body  (Main   times.   delay   boundaries?   of  extension?   of  compression?   of  shearing   mountain   (Main
        Earth   grade).   crustal   the   should   and   List,   crust   or   comments   seismic   boundaries?   areas   ridge?   interpretation.
        Whole   discuss   paper   stage.   this   ridge?   oceanic   rift   grade).   observations.   on   transform   convergent   areas   areas   mid-ocean   collisional   grade).   .
        For   course   of   that   Reference   at   long   changes;   mid-ocean   thin   to   continental   instructor's   seismic   boundaries;   based   and   at   showing   showing   showing   or   or   zone   gravity
        Assignment   5%   papers   observations.  The   Body,   Main   2  pages   velocities.   or   rift   range?   continental   a   al   course   of   the   earthquake   above).   plate   region:   changes   divergent   depth   solutions   solutions   solutions   rift   subduction   course   of   on   based
        Writing   term;   of   three   to   refraction   about   be   available:   now   thickness;   thickness   velocities;   mantle  observations/interpretations:   continental   mountain   thick   velocities   8%   week;   considering   about   available:   now   (see   of  lithospheric   the   in   thickness  observations/interpretations:   at   considerable   plane   plane   plane   focal   continental   a   at   a   at   10%   part   a   available:   now   above).   (see
        Sequenced   week   4th   one   of   seismic   Title,  Abstract,   a   should   constraints   refraction:   crustal   of  crustal   crustal  Internal   Uppermost   a   at   a   at   crust   from   upper-mantle   6th   paper,   papers   constraints   refraction   Positions   of  stresses   Lithospheric   earthquakes   to   focal   fault   focal   fault   fault   lithosphere   lithosphere   week;   8th   adding   constraints   refraction
             (Due   overview   on   including   paper   Seismic   Overall   a)   Pattern   b)   c)   d)   new   Thin   crust   Thick   Transition   margin?   Low   (Due   entire   on   Seismic   Earthquake:   a)   Types   b)   c)   new   Shallow   Earthquakes   Normal   Reverse   Strike-slip   Thin   Thick   (Due   paper.   Seismic
        AppendixA   Iteration   an  Write   based   region   spaced,   of  the   Body   Potential   1.   Potential   ¢   ¢   *   ¢   Iteration   the  Rewrite   based  mation   4  pages).   Potential   1.   2.   Potential   *   ¢   *   ¢   *   ¢   *   Iteration   entire  Revise   pages).   to 7   Potential   1.
        334   First                                    Second   to                                   Third   5
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