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