Dip slip faults in which the hanging wall moves down relative to the footwall are called?
In a normal fault, the hanging wall moves downward, relative to the footwall. A downthrown block between two normal faults dipping towards each other is a graben. An upthrown block between two normal faults dipping away from each other is a horst. Low-angle normal faults with regional tectonic significance may be designated detachment faults.
Dip slip faults in which the hanging wall moves only down relative to the footwall are called?
dip-slip, offset normal fault
Fault (geology)
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Dip slip faults in which the hanging wall moves down and horizontally relative to the footwall are called?
oblique-slip
Fault (geology)
https://en.wikipedia.org/wiki/Fault%20%28geology%29
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.
Fault (geology)
Dip-slip faults can be either normal ("extensional") or reverse.
Fault (geology) Dip-slip faults
A fault which has a component of dip-slip and a component of strike-slip is termed an oblique-slip fault.
Fault (geology) Oblique-slip faults
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Dip-slip faults can be either normal ("extensional") or reverse. In a normal fault, the hanging wall moves downward, relative to the footwall. Dip-slip faults in which the hanging wall moves down and horizontally relative to the footwall are called oblique-slip faults, which hav a component of dip-slip and a component of strike-slip.