10/11/2009 1 Plate Tectonic Theory • Not continental ‘drift’ !! • Importance: – The unifying theory for all other theories in the Earth sciences – Has resulted in a more detailed understanding of Earth history – Has enabled geologists to more precisely (and cheaply) discover new oil, natural gas, and other subsurface natural resource deposits Lithosphere and Asthenosphere Important Definitions • Lithospheric Plate – a large segment of Earth’s crust and upper parts of mantle; extends to top of the low velocity zone • Lithospheric Plate Boundary (Margin) – Divergent - plates move away from one another – Convergen t – plates move toward one another – Transform – plates move horizontally past one another Part I Development of Plate Tectonic Theory Alfred Lothar Wegener (1880-1930)
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10/11/2009
1
Plate Tectonic Theory
• Not continental ‘drift’ !!
• Importance:
– The unifying theory for all other theories in the Earth sciences
– Has resulted in a more detailed understanding of Earth history
– Has enabled geologists to more precisely (and cheaply) discover new oil, natural gas, and other subsurface natural resource deposits
Lithosphere and Asthenosphere
Important Definitions
• Lithospheric Plate – a large segment of Earth’s crust and upper parts of mantle; extends to top of the low velocity zone
• Lithospheric Plate Boundary (Margin)
– Divergent - plates move away from one another
– Convergent – plates move toward one another
– Transform – plates move horizontally past one another
Part I
Development of Plate Tectonic
Theory
Alfred Lothar Wegener (1880-1930)
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Pangaea (Greek, meaning ‘all lands’)
Positions of the continents approximately 200 million years ago
Wegener’s Evidence for Pangaea:
• ‘Fit of the Continents’
– Continental margins fit together like pieces of a jigsaw puzzle
• Paleontological
– Similar fossils on opposite sides of ocean basins
• Geological
– Similar rock types on opposite sides of ocean basins
• Climatological
– Evidence of glaciation in tropical climates
– Fossils of tropical plant species in polar climates
Fit of the Continents Paleontological Evidence
Locations of Mesosaurus fossils
Glossopteris
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Glossopteris
Geological Evidence
Similarity of rock types and ages in the
Appalachian, British Isles and Caledonian
mountain systems
Geological Evidence
Reconstruction of the Appalachian mountain
system at the time it formed, approximately
300 million years ago
Scottish Highlands
Highlands, North CarolinaClimatological Evidence
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Glacial GroovesWhy was Wegener’s idea rejected?
Wegener (left) and an Innuit guide on his last expedition in Greenland.
This is one of the last photographs taken of Wegener, taken shortly
before his death.
Discovery of The Mid-Ocean Ridge System
Mid-Ocean Ridge System
Paleomagnetism – the study of Earth’s
magnetic field as recorded in ancient rocks
Magnetic minerals ‘point’ in the direction of
the magnetic north pole.
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Apparent Polar Wandering: Two North Poles? Apparent Polar Wandering: Single North Pole
Use of Magnetic Minerals to Determine Paleolatitude
Step 1:
Determine Magnetic Dip:
a) 90o (NH)
b) 63o (NH)
c) 37o (NH)
d) 60o (SH)
e) 6o (SH)
Step #2: Determine Paleolatitude
From Magnetic Dip
a)90o N (North Pole)
b)42o N
c)18o N
d)38o S
e)3o S
Cox and Dallrymple: Magnetic Reversals
from all continents record changes in Earth’s
magnetic field at the same time
Cox and Dallrymple: The Magnetic Time
Scale
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Harry Hess: The mid-ocean ridge is a site of
sea floor spreading
Vine and Matthews: Magnetic sea floor
stripes record magnetic reversals
Normal Polarity – exhibited by rocks with
magnetic minerals which ‘point’ towards
today’s position of the magnetic north pole
Reversed Polarity – exhibited by rocks with
minerals which ‘point’ towards today’s
position of magnetic south
As the sea floor spreads, repeated ‘stripes’
of normal and reversed polarity ocean floor
basalts are erupted along the MOR Problem:
What did the theory of sea
floor spreading imply about
the size of the Earth?
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Solution to Problem:
Benioff Zones
Distribution of shallow-, intermediate-, and
deep-foci earthquakes:
Benioff Zones
Part II
The Theory
Types of Lithospheric Plate Boundaries
• Convergent Plate Boundaries
– Characterized by compressive tectonic stress
– Oceanic – continental convent boundary
– Oceanic-oceanic convergent boundary
– Continental-continental convergent boundary
• Divergent Plate Boundaries
– Characterized by extensional tectonic stress
– Oceanic-oceanic divergent boundary
– Continental-continental divergent boundary
Types of Lithospheric Plate Boundaries
• Transform Plate Boundaries
– Characterized by shear tectonic stress
– Continental-continental transform plate
boundary
– Oceanic-oceanic transform plate boundary
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Oceanic-Continental Convergent Plate Boundary
• Subduction of higher density (mafic)
oceanic lithosphere beneath lower density
(felsic) continental lithosphere
– Formation of magma in the mantle wedge
– Formation of a continental margin volcanic arc
on the overriding continental lithosphere
• Examples: Cascade Range, Andean Range
Formation of a subduction zone and continental
margin volcanic arc
Cascade Range Andes Range
Oceanic-Oceanic Convergent Plate Boundary
• Subduction of (mafic) oceanic lithosphere
beneath (mafic) oceanic lithosphere
– Formation of magma in the mantle wedge
– Formation of a volcanic island arc on the
overriding oceanic lithosphere
• Examples: Lesser Antilles, western Aleutians,
Japanese islands
Formation of a subduction zone and
volcanic island arc
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Lesser AntillesAleutian Islands
Japanese Islands Continental-Continental Convergent Plate