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The long-term failure characteristics of overconsolidated clay shales in the Mount Diablo region
AuthorFerrone, Kenneth C.
Geological Sciences and Engineering
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Relatively shallow slides at inclinations comparable to the residual friction angle of the existing clay shales are occurring within Lime Ridge. A stability analyses was preformed on three potential slides to determine some of the failure mechanisms commonly associated with overconsolidated clay shales.
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