Page 352 - Whole Earth Geophysics An Introductory Textbook For Geologists And Geophysicists
P. 352
of
ideas
topo-
DISCUS-
335
mantle.
integration
and
and
Paper
upper
strength?
interpretations
the
basins;
mantle
margins?
of
on
stage.
-
and
bodies;
ranges?
Components
region, based
sedimentary
crust
elevated
basement?
lithospheric
this
continental
magnetic
long.
grade).
mountain
the
ridges?
At
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%
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magnetics
brittle/ductile
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Susceptibility. size, and
thickness
the
tectonic
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distribution;
above).
above).
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week;
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of
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thickness
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add
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Heat
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Iteration
¢
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c)
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¢
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SION
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on
Fourth
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

