Introduction to Earthquakes EASA
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Transcript Introduction to Earthquakes EASA
Lecture #06Plate Motions
Lecture-6
1
Tectonic Plates are Rigid
“Caps” not Flat, Planar Sheets
Lecture-6 2
Plate Motions on a Sphere
Mathematically
speaking, the most general
way to describe the movement of a rigid
plate (cap) on a sphere is through rotation
about a fixed pole
is known as Euler’s Fixed Point
Theorem
The
Lecture-6 3
Plate Motions on a Sphere
The pole of rotation for
plate motion is an
abstract mathematical
concept, it is not a
physical feature. The
point representing the
pole is known as an
Euler pole.
Lecture-6 4
Euler Poles
Euler poles for plate
motions are different than
the geographic North and
South Poles.
The Euler pole for the
motion of a plate is often
“located” on another
plate
Lecture-6 5
Example of Euler pole
describing the relative
motion of Africa from a
fixed, North American
reference frame.
Lecture-6 6
Euler Poles and Ridges
Lecture-6 7
Euler Poles and Ridges/Transforms
Ridge Segments “point”
towards the Euler pole
Corresponding transform
faults are arcs of circles
having the Euler pole as a
center.
Lecture-6 8
GPS Derived Plate Motions
Where is the Euler Pole ?
Lecture-6 9
Relative Plate Motions
It
is important to remember that plate
motions are generally given relative to a
reference frame.
Example:
The half-spreading rate vs. full spreading
rate at a MOR.
Lecture-6 10
Relative Plate Motions
Hypothetical three
plate example: We
know the relative
velocity of B and C;
we also know the
relative velocity of A
and B. What is the
relative velocity of A
and C???
Lecture-6 11
Relative Plate Motions
To
solve this problem we note the basic law
relating relative plate velocities:
aVc
= aVb + bVc
The
velocity of plate C relative to plate A
equals the velocity of plate B relative to
plate A plus the velocity of plate C relative
to plate B.
Lecture-6 12
Remember That Velocities
are Vector Quantities
Lecture-6 13
Remember That Velocities
are Vector Quantities
(This is an example of adding two vectors graphically.)
Lecture-6 14
Solution to Problem
The velocity of plate C relative to plate A has a direction
that is perfectly horizontal, and a magnitude of
(3)(1.414) cm/yr.
Lecture-6 15
Plate Motion Summary
Tectonic plates are spherical caps
The motion of tectonic plates is best
described as rotation about an Euler pole
Plate motion is generally generally given
with respect to a fixed reference frame
The velocities of plate are vectors, they
have a magnitude and direction
Lecture-6 16