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Published byNeil Strickland Modified over 9 years ago
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Thrust Faults
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What kind of fault is it? Precambrian Paleozoic
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How Thrust belts form
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Thrust Belt in a Sandbox
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Parts of a Thrust-Belt
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Components of a thrust belt forethrust Backthrust Basal Detachment Basement
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Origin of Foreland Basins
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Asia Topography
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Sevier Thrust Belt, Wyoming Complex Imbricate fan Basement involved def. Thin-skin def.
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Appalachians
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Sequence of deformation Forward propagation of deformation front 1 1 1 1 2 2 2 3 3
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Canadian Rockies Mountain Front
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Faults of the Canadian Rockies
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Bow and arrow rule
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Distribution of Shortening
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Mt. Yamnuska, Canadian Rockies- McConnell Thrust
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Cretaceous foreland basin strata Cambrian limestone
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Dev. Limestone Palliser Fm. Cretaceous, Belly River Gp. Lewis Thrust
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Folded Paleozoic Rocks of the Sawback ranges
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Front Ranges E W
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E W Rundel Thrust Pz limestone Jur-K Kootenay Fm.
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Detached folds- Jura Mts. Salt Detachment surface
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Calico Bluff, Eagle, AK Pop-up Structure- A Faulted Fold
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Thrust Breaching the Surface- Landers, CA
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Geometry of Thrust Sheets The shape of the fault plane determines the geometry of the folds
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The hanging wall conforms to the shape of the footwall
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Fault-bend-fold Progression
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Thrust belt movie
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Termination of fault-related fold
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Fault-related Folding
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Duplex
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Thrust belt movie
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Duplex Spacing
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Duplex Structure in thin-bedded sandstones and shales
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Fault- propagation fold The fault grows as displacement grows
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Map patterns Complicated due to erosion of the thrust sheets
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Mechanical Paradox of Thrust Sheets Stress required to move a thrust sheet is larger than the strength of the rock Like trying to push a Jell-O block across the table
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Solutions: 1.Reduce Basal Friction High fluid Pressure 2.The sheet does not move all at once
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Role of Fluid Pressure
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Like pushing a wrinkle out of a rug
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Critical Wedge Growth
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Keystone thrust fault, southern Nevada B B D D
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