Plate Tectonics Flashcards

0
Q

Type of earths crust

A

-oceanic
-continental
Most tectonic plates contain both types of crust but some only ocean crust

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1
Q

Basis for Wegeners hypothesis

A
  • the shape of the Atlantic Ocean
  • similarities of fossils and rock sequences on opposite sides of the Atlantic
  • fossils of tropical plants in the arctic
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2
Q

Types of continental margins

A
  • active: margin of a continent is a plat boundary

- passive: margin of continent does not include a plate boundary

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3
Q

Earths upper mantle and crust

A
  • lithosphere: rigid crust + top of mantle

- asthenosphere: partially-molten part of mantle -> source of basalts

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4
Q

Divergent boundaries

A
  • mid-ocean ridges
  • continental rifts
  • in both, new ocean crust is created by basalts and gabbros that originate as magmas in the mantle’s asthenosphere
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5
Q

Features of divergent boundaries

A
  • new ocean crust is created
  • earthquakes are typically small
  • very active basalt volcanism
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6
Q

Convergent boundaries

A
  • island-arc subduction
  • Andean-type subduction
  • continent-continent collision
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7
Q

Island arc subduction

A

Subduction of ocean crust under ocean crust

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8
Q

Andean type subduction

A

Subduction of ocean crust under continental zone

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9
Q

Benioff zone -> earthquake generating zone

A

Earthquakes that are associated with subduction are caused by friction between the sub-ducting plate and the overlying crust or mantle

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10
Q

Features of ocean crust subduction

A
  • consumption of ocean floor
  • large earthquakes
  • explosive volcanism dominated by dacite and andesite lavas
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11
Q

Features of continental collisions

A
  • produce tall, mountain belts

- can produce large earthquakes

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12
Q

Features of transform fault boundaries

A
  • they are offsets in crustal plate boundaries, especially mid-ocean ridges
  • can occur on land
  • no crust is created or consumed
  • can produce large earthquakes
  • volcanism is very rare
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13
Q

Model of a hot spot

A

In the 1960’s J Tuzo Wilson propose the “hot spot” hypothesis
-mantle plumes (hot spots)

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14
Q

Evidence for active plate tectonics

A
  • earthquake distribution
  • volcanic activity
  • direct measurements (GPS, ground-based)
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15
Q

Evidence for past plate tectonics

A
  • fits continental margin
  • match of geological belts in different continents
  • volcanic hot-spot traces
  • flora and fauna at “wrong” latitudes
  • geomagnetic record (paleomagnetism)
  • age of oceanic floor
16
Q

Magnetic polarity in mid-ocean ridge basalts

A
  • discovered in 1962, explain in 1963

- reversals in magnetic field are recoded by magnetite within MORB’s!

17
Q

Magnetic “stripes” at mid-ocean ridges

A
  • magnetic reversals are mirror images in both sides of ridge
  • rocks are progressively older away from ridge
  • > demonstrate the existence of divergent plate tectonic boundary
  • > demonstrate past reversals in the earth’s magnetic field
18
Q

Paleomagnetic measurements

A

-paleodip (paleoinclination): dip of magnetic field along the surface of the earth
-paleodeclination: apparent angle of magnetic field direction N->S (“polar wander”)
This tells us about past rotation of land mass

19
Q

Some plate tectonics influences in climate and evolution

A
  • shifting of continents influences patterns of ocean currents
  • mountain ranges influence weather patterns
  • flora and fauna can take different evolutionary paths on separated continents
  • new continental bridges allow for exchange on species