Chapter 20. Plate Tectonics
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1 Chapter 20 Plate Tectonics
2 Early Evidence (Wegener) The geometric fit of the continents. The similarity in rock age groups between adjoining regions. The similarity in Paleozoic fossils between adjoining areas. The distribution of Paleozoic glaciation in S.America, S.Africa, Australia, and India.
3 The geometric fit of the continents.
4 Similarity of Paleozoic Fossils in adjoining regions.
5 Early Objections Mantle is solid (Transmits S-waves). How can continents move and remain intact? What is the driving force?
6 Polar Wandering Paleomagnetics is the study of rock magnetism. Magnetic minerals in rocks record the direction of the Earth s magnetic field at the time they cool. Each continent gives a different path of the pole. Rocks from the same continent gave the same path.
7 Polar Wandering
8 Magnetic Anomalies Magnetic minerals such as magnetite (Fe 3 O 4 ) record Earth s field. They also perturb the field by a small amount. Perturbations are called magnetic anomalies. Anomalies can be mapped using magnetometers dragged behind aircraft or ships.
9 Magnetic Anomalies Ship-born magnetometers recorded patterns of magnetic anomalies in the North Atlantic (1965-7) Patterns form stripes parallel to Mid-Atlantic Ridge. Stripes are symmetric about the Ridge. Stripes are due to magnetic minerals in the basalt recording the magnetic field at the time of their emplacement.
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11 Magnetic Anomalies Anomalies were first solid evidence of seafloor spreading. Here was a credible hypothesis that demanded testing.
12 Test the Hypothesis Rocks in adjoining parts of Africa and South America were age-dated using new radio-isotopic methods: they matched perfectly. Rocks were dredged from the sea floor: they showed ages symmetrically increasing away from the ridge. There were no old (>250MY) rocks. The fit of continents was revised using the edge of the continental slope rather than the coastline: the match was nearly perfect.
13 Rocks were dredged from the sea floor: They showed ages symmetrically increasing away from the ridge. There were no old rocks (>250MY).
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15 Test the Hypothesis Seismic evidence suggested that crust was being subducted (returned to the mantle) at convergent boundaries to balance crust production at the ridges. Hess proposed a plausible mechanism for the driving force that moved continents: thermal convection in the solid mantle.
16 Theory of Plate Tectonics There appear to be 13 major plates that cover the globe. The plates can contain oceanic, or continental crust or both. New oceanic crust is created at the mid-ocean ridge (divergent boundary). Old oceanic crust is consumed (subducted) at convergent plate boundaries.
17 Deep Earthquakes are only below deep ocean trenches. Velocity structure suggests subduction. Red = slow = hot green = fast = cold
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19 There appear to be 13 major plates that cover the globe.
20 Theory of Plate Tectonics Continental crust resists subduction. Continent-continent convergent boundaries form major mountains. Ocean-ocean and ocean-continent convergent boundaries form subduction zones marked by deep ocean trenches and Benioff Zones (deep earthquake zones extending to 670km).
21 Plate Boundaries Divergent (Ocean - Ocean) Mid Atlantic Ridge: Ocean ridge volcanism Convergent (Ocean - Ocean) Tonga Trench: Island arc volcanism (Ocean - Continent) West Coast of South America: Andesitic to silicic volcanism (Continent - Continent) Alps, Himalayas: Little or no volcanism Transform (San Andreas) Little or no volcanism
22 Divergent and Transform Boundaries
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24 Passive and Active Continental Margins
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