Geological structures Flashcards
(22 cards)
geo structures
natural phenomena of deformed or fractured rock units (strata) in 3D
geology goals (geo structures)
use measurements of rocks to find the history of a deformation and to understand the stress fields causing it
geo engineering goals (geo structures)
use measurements to find stability of deformation, and to predict the future stability
fold
- ben or curved rock strata
- formed due to plastic deformation
fold belt
- set of folds distributed on a regional scale
- common with orogenic zones (mtns)
Components of a fold axial surface -|- / -|- \ / / \ \ limb hinge line fold axis runs parallel the plain of the fold
look at pics for better description
types of folds
-Anticline: upside down U
-Syncline: U
-plunging fold: fold starts out horizontal than the fold axis comes to an angle with the ground called the “angle of plunge”
-basin: dish-like
-dome: …..
-monocline: slight step down in elevation
_________
_____/
horse mountain (He Lan Shan) Chongqing & 3 Gorges
mountains with numerous folds in China
Fault
- planar fracture in a rock
- the rock one side moved with respect to the other.
- can be small to tectonic plate boundaries size
fault zone
series of faults in a zone with complex deformation
Components of a fault
- slip vector: direction of slipping strata
- footwall: the strata that doesn’t move
- hanging wall: strata that does move
types of faults
- normal: where hanging wall slides down decline
- reverse/thrust: hanging wall is pushed up incline
- shear/tear/strike-slip: no change in elevation, just slipping strata passed each other
types of strike slip faults
- sinistral/left-lateral: when viewed from above, strata make ccw motion
- dextral/right-lateral: when viewed from above, makes cw motion
series of faults
- step faults: look like stairs
- block faults: misaligned block shaped faults
- horse/rift valley or graben: trapezoid shaped strata that form valleys above ground
slickensided fault surface
- smoothly polished surface caused by frictional movement between rocks along the two sides of a fault
- striations are the lines in the direction of the sliding on the fault face.
Tension Crack
-opening in the rock due to tensile failure in slope with downward displacement
joints
- planar discontinuities in rock that show or have fracture that aren’t displace with respect to each other
- slight displacement can occur
fissures
- microscopic cracks in rocks that are smaller than joints
- usually don’t have pattern
loading conditions for geo structures
look at page q07-8-9
geo structures in HK
-Fault shown in cliff at ma shi chau
geo structure engineering considerations
- geo structures are internal weaknesses of rocks and sites of penetration/ground water to screw up other foundational sites
- principal stresses are essential for cave/tunnel making
geo structure types
fold fault fracture joint fissure