Stress analysis of a deeply eroded analog of the San Andreas Fault, California
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Geology topics
David L. Kohlstedt
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Stress analysis of deeply eroded analogs of the San Andreas Fault (a renewal)
We have studied deformation-induced microstructures in quartzo-feldspathic rocks from the Nordre Stromfjord shear zone, within the central part of the Nagssugtoqidian mobile belt of West Greenland (Figure 1).
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