Structural Year 2 Exam 2 Flashcards
Hinterland
The direction towards the more deformed
Foreland
Direction towards the undeformed
Allochthonous
The part that is moving
Autochthonous
The part that isn’t moving
Decollement
The stationary, more competent layer under the surface that contributes to the thin-skinned deformation
What is Critical Taper theory
Deformation in the hinterland builds to the critial taper, once reached the thrust sheet moves.
What ways is the critical angle restored?
By forming a thrust fault, eroding the hinterland, and normal faulting caused by gravity
Duplex
Thrust sheet that has a floor thrust and a roof thrust
Free folds
based entirely on physical mechanical properties
forced folds
requires bending and stretching
Fault-bend-fold
The start of a duplex
Forced-propagation-fold
The start of an imbricate fold
Releasing bends
curve in the fold that causes a gap
Restraining bends
curve in the fold that causes bunches
What is the result of releasing bends
extension
normal faults
Grabens/basins
What is the result of Restraining bends
Compression
Reverse faults
uplift/mountains
In a left lateral slip, which direction is the Riedel shear pointed?
Right (opposite)
In a left lateral slip, which direction is the en echelon array pointed?
left
Stratography is known
____cline
Stratography is unknown
____form
Stratography is normal
Young over old
Stratgraphy is not normal and peaks upward
antiformal syncline
Stratography is not normal and peaks downward
synformal anticline
in sequence thrusting
a thrust sequence that has formed progressively and in order in one direction
step over to the left
compression
step over to the right
extension