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STRUCTURE OF THE EARTH (Structure (Continental Crust (Not subducted =…
STRUCTURE OF THE EARTH
Structure
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The Core
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Outer core
Contains liquid Fe, Ni, S
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Oceanic Crust
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Basalt, magma, silicon, Mg: (SIMA)
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Continental Crust
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Granite, Al, Si (silica): SIAL
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Continental Drift
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Alfred Wegner
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Continental fit, rock distribution + ancient glaciation = evidence
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Evidence
Gondawanaland
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S America, Africa, Antarctica, India, Australia
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Broke up in Jurassic period, 167 Ma
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Fit
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Matching sequences of glacial, marine + non-marine rocks found across several continents
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Rock Types
Proof that 2 rock types on either side of ocean are from same outcrop, they must have the same:
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Precambrian cratons, carboniferous coals
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Fossils
If Africa + S Am were always separated, they should have diff. fossil records - esp. for orgs. that would not have been able to spread across a wide ocean
During the Carboniferous, land-based orgs. are found on both continents
Glaciation
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Orientation of striations in bedrock in Aus.. S Am + India suggest glaciers formed in oceans and moved on land
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Paleomagnetism
Iron-rich minerals in magnetic field hold a record of the E's mg. field at the time of their formation
Large no. of rocks collected, dated and direction of the PM measured
Data plotted as a polar wandering curve - the curve joins up the apparent positions of the mg. N over time
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If the 2 continents are repositioned next to each other, the curves match = one position for the pole
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CD + Plate Tectonics
Sea Floor Spreading
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- new rock coming thru ridge pushes old rock on either side along
- the rocks pushed away is the same on either side
- bc of changes in polarity, there is a pattern along the fold mts; there is a ridge in the middle e.g. MA Ridge
- All igneous rocks formed at MA ridges contain iron
- Fe minerals cool as lava erupts
- Fe minerals become aligned with E's m.f.
- Fe minerals is rocks becomes a record of magnetic polarity at the time the rock was formed
- When polarity of rocks formed on each side of ridge was compared, they were found to match
Paleomagnetic Record
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Lava erupts + cools and mg. orientation of Fe particles is locked in the rock, depending on polarity at that time
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