LONG DOES IT TAKE TO REACH A STEADY STATE STRESS? By
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 earth...
Main Authors: | , , , |
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.425.1535 http://lib.uky.edu/ETD/ukymeen2005t00234/newranjiththesis.pdf |