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CHAPTER 2 Plate Tectonics and the Ocean Floor (I)
Instructor: Dr. Dong at ECC
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Layered Earth Fig. 1.14
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Fig. 1.15
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Asthenosphere Upper mantle Plastic—deforms by flowing
High viscosity—flows slowly
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Plate tectonics explains:
Global distribution of Volcanoes Earthquakes Faults Mountain belts Features of seafloor Evolution of continents and oceans
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Exe. 2-1 How many layers in the earth structure?
2. What is the plate tectonic?
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Hypothesis: Continental drift
Wegener proposed one large continent (1912) Pangaea Surrounded by single large ocean Panthalassa About 200 million years ago
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Fig. 2.2
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Evidence for continental drift
Puzzle-like fit of continents Edward Bullard fit continents at 2000m water depth Fig. 2.3
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Evidence for continental drift
Matching sequences of rocks and mountain chains Similar age, rock types, structures
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Figure 2.4a
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Figure 2.4b
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Evidence for continental drift
Glacial ages and other climate evidence Ancient glaciation in modern tropical regions Direction of glacial flow Distribution of organisms Same land animals distributed in different continents (e.g., South America and Africa)
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Fig. 2.5
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Fig. 2.6
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Objections to continental drift
Continents cannot “plow” through ocean crust Gravitational forces associated with tides too small
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Exe. 2-2 List evidences to support the continental drift
Why was the continental drift a hypothesis?
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Evidence for plate tectonics
Earth’s magnetic field Paleomagnetism Magnetic alignment (N or S) Magnetic inclination (magnetic dip) Latitude
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Fig. 2.7
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Apparent polar wandering
Pangaea Fig. 2.8
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Magnetic polarity reversals
Fig. 2.9
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How is earth’s magnetic field used for the tectonic plate?
Exe How is earth’s magnetic field used for the tectonic plate?
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Sea floor spreading Harry Hess (1962)
Mid-ocean ridge site of new ocean crust Oceanic trench site of crust destruction (subduction) Fig. 2.10
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Evidence to support sea floor spreading
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Earth’s magnetic polarity as sea floor created
1. Parallel magnetic anomalies record changes in Earth’s magnetic polarity as sea floor created Fig. 2.11
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2. Age of ocean floor increases away from crest of mid-ocean ridge
Fig. 2.12
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3. Global distribution of earthquakes
Fig. 2.13
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Evidence to support sea floor spreading
Parallel magnetic anomalies record changes in Earth’s magnetic polarity as sea floor created Age of ocean floor increases away from crest of mid-ocean ridge Most large earthquakes occur along plate margins
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Fig. 2.10
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Plate tectonics theory
Lithospheric plates “float” on the asthenosphere Large scale geologic features occur at plate boundaries Two major tectonic forces Slab pull Slab suction
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Exe List evidences to support plate tectonic theory.
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