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Lecture 6 Normal faults 2
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Normal faults Tectonic environments (5) Landscapes (6) Coseismic structures and patterns (6) –Case history from Nevada, 1954 –Case history from Idaho, 1983
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from MacQuarrie and Wernicke (2005)
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Some landforms: Triangular facets, alluvial aprons, wineglass canyons, and turtlebacks
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Fault ribbons, alluvial aprons and triangular facets
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Triangular facets, wine-glass canyons, and slumps
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Turtlebacks
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Sparta
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Mani
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A “brick” (or two) The “Building” Mani peninsula, Greece
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Mycenae
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Orem Ephesus
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Faulting versus dike intrusion in the Mono Basin, eastern California
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Calculation of slip rates ~25m/15,000 years McGee Creek, eastern Sierra Nevada
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A Case History: Ruptures of the Dixie Valley and Fairview Peak earthquakes, 1954
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Historical ruptures in the Central Nevada Seismic Zone Irregularity of fault plane in direction perpendicular to slip vector
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Stillwater rangefront
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A Case History: Rupture of the Lost River Range fault during the Borah Peak earthquake, Idaho, 1983
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Geometry of the fault rupture
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A detail of the rupture
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Coseismic slip function
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Vertical coseismic deformation
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Coseismic vertical deformation profile Aftershock cross-section Geologic cross-section
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