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Published byRoxanne Boyd Modified over 9 years ago
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Normal Faults Extensional Tectonics
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Tectonic Settings for Extension Divergent plate motions Gravitational collapse –Over-thickened crust –Continental margins Salt Domes
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Extensional Tectonics
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Divergent Boundary Normal Faults, rifts
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Continental Extension
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Divergent Boundaries Continental Plate Separation East African Rift Valley Somali Subplate African Plate Parallel valleys; volcanoes and earthquakes.
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Rifts Bounded by normal faults
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Back Arc extension
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Extension of the lithosphere 1
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Extension of the lithosphere 2
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Lithospheric Extension Thinning of the lithosphere Normal faulting at the surface High heat flow (rinsing of the isotherms) Thermal subsidence - > sedimentary basins
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North Sea Extensional Basin
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Pure shear vs. simple shear systems
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Gravitational Collapse of Mt. Belts
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Basin and Range Province
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New Mountains-Active Fault –Basin and Range Province
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Two modes of extension
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Sandbox- Block rotation Sand above plasticine
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Block Rotation
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Domino block rotation in the Basin and Range
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Listric (curved) Faults- roll over anticlines
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Small roll-overs
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Sedimentation during faulting Growth faulting AnimationAnimation by R. Allmendinger http://www.geo.cornell.edu/geology/faculty/RWA/movies/
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Curved faults – Block rotation Growth Strata 3 km 0
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Gulf of Mexico
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Passive Margin
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Gulf of Mexico Salt
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Extension Above Salt Diapir
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Transfer zone in a rift
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Older faults rotate and become inactive New faults cross-cut them Result= large magnitude extension Successive generations of normal faults
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