Folds

folds
What is fold?


- Undulations or waves in rocks formed by stratified formation such as sedimentary and volcanic rocks or either metamorphosed equivalents.
1- Axial plane: the plane that divides the fold symmetrically as possible and includes hinge line
2- ¨Hinge line: line formed by the intersection of axial plane and curved part of fold
May be classified according to:
Shape (straight , curved , irregular)
Position (verticle , inclined , horizontal)
3- Limbs: the two sides of a fold that are divided by axial plane
4- Hinge point: the point of maximum curvature of a fold
5- Fold axis: the geometric lines on both sides of fold that are parallel to hinge line
6- Axial trace : the line produced by intersection of axial plane and any other plane



Based on shape: 
¨Anticline fold: convexing upward and has older rocks in the core
¨Syncline fold: concaving upward and has younger rocks in the core 
¨Synform  anticlinars e: it appesyncline but it has older rocks in core like anticline fold
•      Dome form: layers dip in all directions  away from the central point
•      Basin form: layers dip inward toward central point
•      Monocline: local steepening with homocline
•      chevorn

Based on tightness (Fleuty classification):

•      Gentle fold : 170 : 180
•      Open  fold   : 90 : 170
•      Tight fold     : 10 : 90
•      Isoclined fold : 0 : 10

Based on scale:

  folds can present in all scales:-
   1-Microscopic (require magnification)
   2-Mesoscopic  (specimen and outcrop size)
   3-Macroscopic(larger scale)


•    Fold orders:
First order : largest fold in given area
Second order : smaller folds found on the limbs of first order fold

Mechanism of fold
•      Folds : are the signatures of deformation forces that result from plate tectonic. The term fold implies that an originally planer structure, such as sedimentary bed, has been bent
•      In plate tectonic(convergence) continental with continental will not occur subduction but occur colloid to each other forming mountain range of folded rocks.                                        
•      Another example of convergence of plat
•      tectonic: oceanic with oceanic , in it will occur subduction among the two layers.


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