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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Bibliographic Details
Main Author: Ravi, Lokranjith K
Format: Text
Language:unknown
Published: UKnowledge 2005
Subjects:
Online Access:https://uknowledge.uky.edu/gradschool_theses/338
https://uknowledge.uky.edu/cgi/viewcontent.cgi?article=1341&context=gradschool_theses