CYCLE-UP OF MULTIPLE RIFTING EVENT MODELS: HOW LONG DOES IT TAKE TO REACH A STEADY STATE STRESS?
Many geological numerical models are initiated with a background stress state of zero. Often these numerical results are compared directly to geodetic data. Recent work (Kenner and Simons, 2004) has shown that modeled deformation rates can change as the model is cycled-up following repeated earthqua...
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| Format: | Others |
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UKnowledge
2005
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| Online Access: | http://uknowledge.uky.edu/gradschool_theses/338 http://uknowledge.uky.edu/cgi/viewcontent.cgi?article=1341&context=gradschool_theses |