Footwall Deformation and Structural Analysis of the Footwall of the Willard Thrust Fault, Northern Wasatch Range, Utah
Deformation mechanisms in the footwall of the Willard thrust fault, northern Wasatch Range, Utah, change from dominantly plastic to dominantly cataclastic (both microscopically and macroscopically) in the Ophir Formation and Maxfield Limestone before the thrust begins to ramp laterally upsection sou...
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| Format: | Others |
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DigitalCommons@USU
1989
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| Online Access: | https://digitalcommons.usu.edu/etd/5784 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=6849&context=etd |