Transcript PLATE TECTONICS - UA Geosciences

PLATE TECTONICS
Last chapter in Davis and Reynolds
OUTLINE OF LECTURE
Plate kinematics
1. In 2-D
2. On a sphere
3. Continental break-up
What drives plate motion?
• Most people agree that plates are intimately
related to mantle convection;
• Slab pull?
• Ridge push?
• Mantle drag
Model linking subduction to plume magmatism
Basic kinematic elements
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Plate boundaries, triple junctions
Absolute plate motion, relative plate motion
Euler poles
Worked examples
Ridges, trenches, transforms
Triple junctions, quadruple j’s
3riple junctions are stable; more plates at a point - not stable
Absolute plate motions - velocity in an absolute reference
frame- say relative to a point outside the Earth. Or an
assumed stationary long lived plume…. E.g. Hawaii
Otherwise, one uses a relative velocity reference frame.
One plate is kept stationary; the velocity of the others
relative to the “stationary” plate is monitored. The
understanding is that the entire system (including the
stationary plate) is actually moving on the globe.
In the case of ridges, we use the half spreading rate for
velocity calculations.
Absolute framework - consider Hawaii a stationary plume
(it delivers melts in exactly the same spot over its entire
history). We can calculate the velocity vector of the Pacific
plate.
75-43 - N20W x cm/yr
; 43-0 Ma N70 W, y cm/yr.
There are very few such long lived plume products and it is
questionable whether they remain fixed. The common way of
tracking plate motions is in a relative framework.
Some useful rules: 1. Plate motions are transform parallel;
2. Plate moves away from ridge
3. The sum of relative plate velocities is zero*.
*- that is because by definition plates are rigid.
Velocity is a vector: magnitude, direction and sense.
Examples
2.
1
Worked exercise
It’s a right lateral transform boundary
Finding the relative
velocity of Farallon to
North America
Complicating a bit- what if the transforms are curved?
We then have to admit there’s some rotation involved.
Any rotation is achieved around a pole. From geometry, this
is called the Euler pole. Transforms form arcs that are
segments of circles centered in the Euler pole of a plate.
Euler poles
Example : Australia and New Zeeland
QuickTime™ and a
Cinepak decompressor
are needed to see this picture.
Plate tectonics on a sphere
• Angular velocity, linear velocity
• Rotations around Euler poles
• Projections on stereonets
Tectonics on a sphere requires that we use angular velocities
v/r and r = R sin g where R is the radius of the Earth.
So what? Check out the fig - predicts motion away
from Euler pole. In this case - 2 plates with E at N
pole
Find distances on a sphere; use lat long and g
The projections used in 3D plate tectonics are
stereonets - equal area - however unlike your usual
down view with geo structures, this is a side view. All
calculations (angles etc) are similar.
What you need to know:
• The fundamentals of plate tectonics, driving
forces; link to mantle convection;
• Differences between present day and past
characteristics of PT;
• Be able to handle simple 2-3-4-… plate geometry
problems in 2D involving only translations.
• Calculate velocity vectors for such examples;
• Know what the Euler pole is and angular vs. linear
velocity. Be able to find one if you have the other.
Continental break-up
• Plume-driven
• Plate-driven
Continental break-up: plumecaused?
Sometimes clearly not. Other
times, major oceans appear to
form during times of major
flood basalts -short lived,
vigorous plume heads that may
have broken the continents apart
Topography of ocean basins
Oceanic basins form
via rifting old
continental margins
Tectonic style is similar to
continental extension,
except the extension is
much higher, > 500%
Example: the Red Sea
Development of passive vs active margins
The anatomy of the passive North American margin