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Structural Geology
Amity School of Engineering and Technology
Structural geology
• Branch of geology that deals with classification, mechanism
and causes of development of rock structures.
 Primary structure
 Structural features that are developed in the body of a rock
during its formation stage.
 Secondary structure
 Modification of original structures and development of new
forms, shapes, alteration of mineral composition induced in rock
after rock formation.
Amity School of Engineering and Technology
Basic terms
• Outcrop
 Exposure of a solid rock on the surface of the earth
• Bedding or stratification
 Layered structure of rock
• Strike
 is the direction of the line that is formed by the intersection
of the rock’s bedding planes with a horizontal surface.
Basic terms
Dip
Max angle of inclination of a layer of a rock with horizontal plane.
Measured using clinometer and compass.
Basic terms
Eldorado Canyon, south of Boulder
Garden of the Gods, Colorado Springs
• Outcrop dimension
– Width, thickness, depth, dip & strike
• Structural form of igneous rock
– Intrusions
• Injection of magma into pre-existing rock
– Flows
• Rock structure formed out of solidified lava on the surface of earth
– Masses
• Enormous bodies of igneous rocks having irregular structural shape
Basic terms
Folds and Folding
Folds are undulation or bend developed in rock under stress
Process of development of folds in rocks is called folding
Parts of fold
Parts of fold
Limbs
 Sides or flanks of a fold
Hinge
 Point where curvature is max., one limb ends and other limb starts
 Line joining all hinge points is called hinge line
Axial plane
 Imaginary plane passing through all points of maximum curvature
Axis of fold
 Line drawn parallel to hinge line
 Line represents the intersection of axial plane of a fold with any
bed of the fold
Plunge of fold
 Angle of inclination of fold axis with horizontal
Crest
 Highest point in up arched crest
Trough
 Lowest point in an down arched fold
Classification of folds
• Anticlines
 Up arched strata, convex upward
 Older rock occupy interior of fold
 Limbs dip away from axial center
• Synclines
 Down arched strata, convex downward
 Younger rock is core of fold
 Limb dip towards a common center
Classification of folds
Parameters for Classification of folds
Position of axial plane
Degree of compression
Behavior with depth
Relative curvature of outer & inner arcs
Plunge of folds
Profile of outer surface
Mode of occurrence
Position of axial plane
Symmetrical folds
Asymmetrical folds
Overturned folds
Isoclinal folds
Recumbent folds
Amity School of Engineering and Technology
Degree of compression
Closed folds
Open folds
Behavior with depth
Concentric folds
Similar folds
Supratenuous folds
Amity School of Engineering and Technology
Relative curvature
Class 1 fold
Class 2 fold
Class 3 fold
Amity School of Engineering and Technology
Plunge as basis
Plunging fold
Non-plunging fold
Amity School of Engineering and Technology
Profile of fold surface
Cheveron folds
Conjugate folds
Cuspate folds
Cylindrical folds
Amity School of Engineering and Technology
Mode of occurrence
Anticlinorium
Synclinorium
Domes and basins
Amity School of Engineering and Technology
Causes of folding
Folding due to tangential compression
Flexural folding
Flowage folding
Shear folding
Folding due to intrusion
Folding due to differential compression
Amity School of Engineering and Technology
Engineering Consideration
Presence of fold need to be given due importance in structures
 Traffic or hydropower tunnels
 Site selection for dam & reservoirs
 Fixing alignments of roads, bridges & highways
Characteristics of folds
 Change in attitude
 Shattering of rock
 Strained nature
Amity School of Engineering and Technology
Thank You
Amity School of Engineering and Technology

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4. lecture on structural geology folds

  • 1. Structural Geology Amity School of Engineering and Technology
  • 2. Structural geology • Branch of geology that deals with classification, mechanism and causes of development of rock structures.  Primary structure  Structural features that are developed in the body of a rock during its formation stage.  Secondary structure  Modification of original structures and development of new forms, shapes, alteration of mineral composition induced in rock after rock formation. Amity School of Engineering and Technology
  • 3. Basic terms • Outcrop  Exposure of a solid rock on the surface of the earth • Bedding or stratification  Layered structure of rock • Strike  is the direction of the line that is formed by the intersection of the rock’s bedding planes with a horizontal surface.
  • 4. Basic terms Dip Max angle of inclination of a layer of a rock with horizontal plane. Measured using clinometer and compass.
  • 5. Basic terms Eldorado Canyon, south of Boulder Garden of the Gods, Colorado Springs
  • 6. • Outcrop dimension – Width, thickness, depth, dip & strike • Structural form of igneous rock – Intrusions • Injection of magma into pre-existing rock – Flows • Rock structure formed out of solidified lava on the surface of earth – Masses • Enormous bodies of igneous rocks having irregular structural shape Basic terms
  • 7. Folds and Folding Folds are undulation or bend developed in rock under stress Process of development of folds in rocks is called folding
  • 9. Parts of fold Limbs  Sides or flanks of a fold Hinge  Point where curvature is max., one limb ends and other limb starts  Line joining all hinge points is called hinge line Axial plane  Imaginary plane passing through all points of maximum curvature
  • 10. Axis of fold  Line drawn parallel to hinge line  Line represents the intersection of axial plane of a fold with any bed of the fold Plunge of fold  Angle of inclination of fold axis with horizontal Crest  Highest point in up arched crest Trough  Lowest point in an down arched fold
  • 11. Classification of folds • Anticlines  Up arched strata, convex upward  Older rock occupy interior of fold  Limbs dip away from axial center • Synclines  Down arched strata, convex downward  Younger rock is core of fold  Limb dip towards a common center
  • 13. Parameters for Classification of folds Position of axial plane Degree of compression Behavior with depth Relative curvature of outer & inner arcs Plunge of folds Profile of outer surface Mode of occurrence
  • 14. Position of axial plane Symmetrical folds Asymmetrical folds Overturned folds Isoclinal folds Recumbent folds Amity School of Engineering and Technology
  • 15. Degree of compression Closed folds Open folds
  • 16. Behavior with depth Concentric folds Similar folds Supratenuous folds Amity School of Engineering and Technology
  • 17. Relative curvature Class 1 fold Class 2 fold Class 3 fold Amity School of Engineering and Technology
  • 18. Plunge as basis Plunging fold Non-plunging fold Amity School of Engineering and Technology
  • 19. Profile of fold surface Cheveron folds Conjugate folds Cuspate folds Cylindrical folds Amity School of Engineering and Technology
  • 20. Mode of occurrence Anticlinorium Synclinorium Domes and basins Amity School of Engineering and Technology
  • 21. Causes of folding Folding due to tangential compression Flexural folding Flowage folding Shear folding Folding due to intrusion Folding due to differential compression Amity School of Engineering and Technology
  • 22. Engineering Consideration Presence of fold need to be given due importance in structures  Traffic or hydropower tunnels  Site selection for dam & reservoirs  Fixing alignments of roads, bridges & highways Characteristics of folds  Change in attitude  Shattering of rock  Strained nature Amity School of Engineering and Technology
  • 23. Thank You Amity School of Engineering and Technology