lecture 3.2 - Deformational structures (brittle + faults) Flashcards
define undeformed rocks
lateral continuity layers (beds)
describe the principle of superposition
the layer underneath the superior layer = oldest layer
oldest layer = 1 in ascending older
define stress
application of forces to a rock layer
define strain
deformation of a rock layer due to stress
What are the 3 types of stress? Define them
compression - opposing forces directed towards each other (–> . <–)
Tension - opposing forces directed against each other (<– . –>)
Shear - forces sliding past each other (–>
<–)
what are the 3 types of strain? Define them
Elastic - rock deforms when stress is present, but returns to OG shape after stress is gone
Plastic - rock deforms while stress is present and stays deform after stress is gone
Brittle - Rock “fractures” and breaks into pieces to relieve stress
What strain deformation are seen in faults
brittle deformation
convergent margin is what stress
compression
divergent margin is what stress
tension
transform fault is what stress
shear
relationship between stress vs. strain
stress –> strain
Head block vs. Foot block
Head = area above fault
Foot = area below fault
Name both types of faults and compare them.
Normal fault = Hanging (head) block falls down relative to Foot block
Reverse fault = Hanging (head) block moves up relative to Foot block
How do we know which block is moving?
we don’t. Assume head block moves and foot block stays stationary
How to identify normal fault vs. reverse fault?
Normal fault = tension = gap in bed (region extended)
Reverse fault = compression = overlap in bed (region shortened)