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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Format: | Thesis Electronic Book |
Language: | English |
Published: |
2015
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Internet
This item is not available through BorrowDirect. Please contact your institution’s interlibrary loan office for further assistance.Stanford University
Call Number: |
3781 2015 N INTERNET RESOURCE |
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