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| | Rift Basin Architecture & Evolution (Site not responding. Last check: 2007-11-05) |
 | | Basin inversion occurs in a variety of tectonic environments (e.g., Buchanan and Buchanan, 1995), including several passive margins related to the breakup of Pangea (e.g., Doré and Lundin, 1996; Vagnes et al., 1998; Withjack et al., 1995, 1998; Hill et al., 1995; Withjack and Eisenstadt, 1999). |
 | | Although the inversion is obvious in this model, erosion of material down to the level of the red line would remove the most obvious evidence of inversion in the half graben. |
 | | Thus, the end of rifting, the initation of inversion, and probably the initiation of seafloor spreading are diachronous along the central Atlantic margin (i.e., during earliest Jurassic time in the southeastern United States and Early to Middle Jurassic time in the northeastern United States and Maritime Canada) (Withjack et al., 1998). |
| www.ldeo.columbia.edu /~polsen/nbcp/breakupintro.html (3417 words) |
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