Chapter 8- Structural Geology Flashcards
(36 cards)
bed
a unit of sedimentation which can vary in thickness
bedding planes
mark the break between beds
dip
maximum inclination of a bed measured from the horizontal using a clinometer
true dip
the actual angle of dip measured at right angle to te strike
strike
horizontal line on a bedding plane, measured as a bearing from north using a compass
apparent dip
a dip that is measured to be less than the maximum
true thickness
thickness of the bed measured at right angle to the bedding planes
apparent thickness
thickness of the bed measured as seen at the outcrop but not at right angle to the bedding plane
fault
fracture in a rock along which there had been an observable displacement
fault plane
plane of fracture along which the rocks have been displaced
upthrow
side of the fault where the movement is upwards, relative to the other
downthrow
side of the fault where movement is downward in relation to the other side
throw
vertical displacement of rocks along a fault plane
footwall
the side of the fault that lies below the fault plane, if the fault is not vertical
hanging wall
side of the fault that lies above the maximum inclination of the fault plane as measured from the horizontal
dip-slip fault
movement along the fault plane is parallel to the dip of the fault plane
normal faults
the hanging wall is the downthrow side
horst and graben
series of normal faults
horst is elevated, graben is dropped
reverse faults
formed by compressional forces
hanging wall is the upthrow side
thrust fault
type of reverse fault where the fault dip is less than 45
strike slip fault
faults where the fault plane is vertical or near vertical and movement along the fault plane is horizontal
tear fault
result of shearing forces applied to rocks
slickensides
striations and polishing found on a fault plane indicative of relative movement
fault breccia
composed of fragments produced by rocks fracturing during faulting, found along fault planes