Fault-related deformation within the brittle-ductile transition field observations, microstructural analysis, and mechanical modeling /

The "brittle-ductile transition" is an interval of Earth's crust where the primary mechanism of rock deformation gradually changes from brittle fracturing to viscous flow with increasing depth. Fault-related deformation within this transitional zone significantly influences earthquake...

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Bibliographic Details
Main Author: Nevitt, Johanna Marjorie
Corporate Author: Stanford University Department of Geological and Environmental Sciences
Other Authors: Pollard, David D (Thesis advisor, primary advisor.), Segall, Paul, 1954- (Thesis advisor, advisor), Warren, Jessica (Jessica Mendelsohn) (Thesis advisor, advisor)
Format: Thesis Electronic Book
Language:English
Published: 2015

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Stanford University

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Call Number: 3781 2015 N
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