any surface with measurable slip; discontinuity in a displacement field
faults
slip occurs on several faults within a band of definable width
fault zone
regions of localized but continuos ductile displacement
ductile faults
fracturing, crushing, and frictional sliding of grains of rock
cataclasis
Anderson’s Theory of Faulting
1 of the 3 principal stresses must be perpendiculat to the surface
fault block beneath the fault surface
foot wall
fault block above the fault surface
hanging wall
relative offset of points once adjacent
displacement
where a feature in the footwall is cut
footwall cut-off
where a feature in the hanging wall is cut
hanging wall cut-off
rocks that have been translated great distances
allochthonous
rocks that have retained their location
autochthonous
locally transported rocks
paraautochthonous
geomorphic feature formed by the offset in a fault
fault scarp
fault that intersected the surface
emergent fault
fault that did not break the surface
blind faults
largest fault in a zone
master fault
dips toward the main fault
antithetic fault
dips in the same direction as the fault
synthetic fault
high angle, down-dip, extensional
normal
low angle, up-dip, contractional
reverse
where do normal faults form in
rifts, passive margins, mid-ocean ridges
relay or parallel arrays
half-graben
fault that decreases dip with depth, concave upward
listric fault