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| | GEOL 102 Orogenesis II (Site not responding. Last check: 2007-11-02) |
 | | The sequence of events (and resulting lithologies) described last lecture has been called a Supercontinent Cycle (or a Wilson Cycle, after J. Tuzo Wilson, who linked spreading centers and subduction zones). |
 | | They represent the union of plate tectonics, orogenesis, volcanism, sedimentology, and other aspects of both continental and oceanic lithospheric geology (and ultimately links to mantle and, presumably, core geophysics). |
 | | Wilson Cycles have been in operation since the origin of modern-style tectonics, and will operate as long as the core continues to generate sufficient heat (i.e., as long as its fissionable "fuel" holds out). |
| www.geol.umd.edu /~tholtz/G102/102oro2.htm (113 words) |
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