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1 EPS 122: Lecture 3 – Plate rotations and velocities Plate rotations and velocities Reading: Fowler Ch 2 EPS 122: Lecture 3 – Plate rotations and velocities Plate boundaries

Plate rotations and velocities Plate boundaries

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EPS 122: Lecture 3 – Plate rotations and velocities

Plate rotations and velocities Reading: Fowler Ch 2

EPS 122: Lecture 3 – Plate rotations and velocities

Plate boundaries

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EPS 122: Lecture 3 – Plate rotations and velocities

Plate velocities A flat Earth

AvB The velocity of plate B with respect to plate A

AvB = - BvA

Mid-ocean ridges: • Also called spreading centers • The half spreading rate is the spreading

rate on one side of the ridge

Subduction zones: • Carat points down dip • Velocity vector on subducting

plate

Transform faults: • Also called strike-slip faults • Right- or left-lateral

• Drawn with half arrow heads

EPS 122: Lecture 3 – Plate rotations and velocities

Calculating relative plate velocities A flat Earth

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EPS 122: Lecture 3 – Plate rotations and velocities

Calculating relative plate velocities A flat Earth

CvB = ?

EPS 122: Lecture 3 – Plate rotations and velocities

Calculating relative plate velocities A flat Earth

CvB = ?

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EPS 122: Lecture 3 – Plate rotations and velocities

Latitude, longitude, great and small circles Rotation poles and vectors

Latitude

• small circles

• on a plane perpendicular to the Earth’s rotation pole

Longitude

• great circles

• pass through rotation pole

• on a plane that contains the rotation axis

EPS 122: Lecture 3 – Plate rotations and velocities

Euler Euler’s fixed point theorem:

“The most general displacement of a rigid body with a fixed point is equivalent to a rotation about an axis through that fixed point”

…a plate is a rigid body

…if the earth is spherical, plates rotate around the center of the Earth

Therefore, any displacement of a fixed point on the surface of the Earth can be represented a rotation about a suitably chosen axis passing through the center of the Earth

Bullard et al, 1965

rotation axis

rotation pole

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EPS 122: Lecture 3 – Plate rotations and velocities

Angular velocity

2D

3D

Right-hand rule

A reminder….

EPS 122: Lecture 3 – Plate rotations and velocities

Plate velocity

plate velocity:

v = R sin

Average radius of the Earth R = 6371 km

Plate velocity depends on the angle from the rotation axis

When quoting plate velocities, give the velocity at 90° i.e. the maximum

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EPS 122: Lecture 3 – Plate rotations and velocities

Strike of transform faults Measuring present day plate motions

Provides location of poles orientation of rotation vector

EPS 122: Lecture 3 – Plate rotations and velocities

Strike of transform faults Measuring present day plate motions

Provides location of poles orientation of rotation vector

Can we obtain pole location from this data?

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EPS 122: Lecture 3 – Plate rotations and velocities

Strike of transform faults Measuring present day plate motions

Provides location of poles orientation of rotation vector

Can we obtain pole location from this data?

…start to see problems

EPS 122: Lecture 3 – Plate rotations and velocities

Variation in spreading rate Fit data to obtain rotation vector

i.e. pole location and rotation velocity

Measuring present day plate motions

plate velocity:

v = R sin

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EPS 122: Lecture 3 – Plate rotations and velocities

Focal mechanism from earthquakes

Provides location of poles orientation of rotation vector

Measuring present day plate motions

EPS 122: Lecture 3 – Plate rotations and velocities

Plate boundary motions

1906 San Andreas

1995 Kobe, Japan

San Andreas at San Juan Bautista, California - Today

Measuring present day plate motions

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EPS 122: Lecture 3 – Plate rotations and velocities

Wallace Creek A record of plate motion

Measuring present day plate motions

EPS 122: Lecture 3 – Plate rotations and velocities

Wallace Creek Measuring present day plate motions

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EPS 122: Lecture 3 – Plate rotations and velocities

Wallace Creek Measuring present day plate motions

EPS 122: Lecture 3 – Plate rotations and velocities

Wallace Creek

= 34 mm/yr

Measuring present day plate motions

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EPS 122: Lecture 3 – Plate rotations and velocities

Matt d’Alessio

EPS 122: Lecture 3 – Plate rotations and velocities

Northern CA

Time till LA reached SF:

Los Angeles: on the Pacific Plate

San Francisco: on the North American Plate

500 km

5 cm/yr = 10 million years

LA

Total Pacific-North America plate motion:

50 mm/yr

Daily GPS observations

Measuring present day plate motions

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EPS 122: Lecture 3 – Plate rotations and velocities

d’Alessio et al, 2005

EPS 122: Lecture 3 – Plate rotations and velocities

Satellite based observations Daily GPS observations

Slope gives average velocity of station to the north

SCIGN – southern CA

Total Pacific-North America plate motion:

50 mm/yr

Measuring present day plate motions

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EPS 122: Lecture 3 – Plate rotations and velocities

NUVEL-1A Measuring present day plate motions

Combine multiple observations and solve for best-fitting rigid plate motions

• 277 ridge spreading rates – use distance of last magnetic

reversal from ridge

• 121 ocean transform-fault azimuths

• 724 earthquake slip vectors

Eurasia fixed

EPS 122: Lecture 3 – Plate rotations and velocities

NUVEL-1A Comparison with GPS observations

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EPS 122: Lecture 3 – Plate rotations and velocities

Global plate motion modeling Seismicity

Seismicity Plate geometry

…problems

Global distributions of continuous GPS