Chapter 9 Flashcards
Deformation of Rocks
Structural geology
Study of the deformation pf rocks (shape, volume, position, orientation)
Stress
Force per unit area. Compressional (convergent plate boundaries, shortening, folding), tensional (divergent plate boundaries, extension, faulting) or shear (transform plate boundaries)
Strain
Change in shape of a rock when stress is applied.
Elastic behavior
Material returns to its original shape when stress is removed. Occurs up to a maximum value of strain, called the elastic limit. (rocks = 0.001)
Plastic behavior
Material does not return to its original shape when stress is removed, behaves as a very viscous liquid.
Primary structures
Happen during rock formation (strata, cross bedding, ripple marks, mud-cracks, graded beds)
Secondary structures
Happen after rock is formed (folds, faults, fractures)
Differential stress
When the force is not the same in each direction
Brittle deformation
Elastic deformation followed by limited plastic deformation. Lower temperatures/pressures (near surface) and high strain rates (fast deformation). Crystalline igneous rocks more susceptible, forms joints and faults.
Ductile Deformation
Plastic strain at constant stress. Higher temperatures/pressures (deeper/close to magma) and low strain rates (slow deformation). Weaker and layered (sedimentary & metamorphic) rocks, forms folds.
Strike direction
Intersection of a horizontal plane with an inclined plane.
Dip angle
Maximum angle of an inclined plane.
Anticline fold
Concave downwards (arch)
Syncline fold
Concave upwards (saucer)
Axial plane
Axis of symmetry with limb on each side
Axis
Intersection of axial plane and a particular rock layer.
Plunge
Difference in angle between horizontal and axis
Folds
Geologic structure that is formed by layers or beds of rock being bent. Visible by outcrops or seismic reflection.
Upright folds
Symmetric, vertical axial plane, limbs dip at same angle in opposite directions
Inclined folds
Asymmetric, axial plane not vertical, limbs dip at different angles in opposite directions
Overturned folds
Asymmetric, axial plane not vertical, limbs dip at different angles in same direction
Joints
Fractures along which no displacement has occurred, occurs in igneous and sedimentary rocks
Faults
Fractures along which displacement has occurred. Classified by strike, dip, slip.
Dip-slip faults
Slip is parallel to dip. Hanging wall located above, footwall located below.