Plate Tectonics Flashcards
(20 cards)
Type of earths crust
-oceanic
-continental
Most tectonic plates contain both types of crust but some only ocean crust
Basis for Wegeners hypothesis
- 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
Types of continental margins
- active: margin of a continent is a plat boundary
- passive: margin of continent does not include a plate boundary
Earths upper mantle and crust
- lithosphere: rigid crust + top of mantle
- asthenosphere: partially-molten part of mantle -> source of basalts
Divergent boundaries
- 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
Features of divergent boundaries
- new ocean crust is created
- earthquakes are typically small
- very active basalt volcanism
Convergent boundaries
- island-arc subduction
- Andean-type subduction
- continent-continent collision
Island arc subduction
Subduction of ocean crust under ocean crust
Andean type subduction
Subduction of ocean crust under continental zone
Benioff zone -> earthquake generating zone
Earthquakes that are associated with subduction are caused by friction between the sub-ducting plate and the overlying crust or mantle
Features of ocean crust subduction
- consumption of ocean floor
- large earthquakes
- explosive volcanism dominated by dacite and andesite lavas
Features of continental collisions
- produce tall, mountain belts
- can produce large earthquakes
Features of transform fault boundaries
- 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
Model of a hot spot
In the 1960’s J Tuzo Wilson propose the “hot spot” hypothesis
-mantle plumes (hot spots)
Evidence for active plate tectonics
- earthquake distribution
- volcanic activity
- direct measurements (GPS, ground-based)
Evidence for past plate tectonics
- 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
Magnetic polarity in mid-ocean ridge basalts
- discovered in 1962, explain in 1963
- reversals in magnetic field are recoded by magnetite within MORB’s!
Magnetic “stripes” at mid-ocean ridges
- 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
Paleomagnetic measurements
-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
Some plate tectonics influences in climate and evolution
- 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