Chapter 9 Flashcards
Deformation
process by which rocks bend, break, or flow in response to “stress” (compression, tension, or shear- ing)
Deformation produces
joints (cracks), faults (fractures on which one body of rock slides past another), folds (bends, curves, or wrinkles of rock layers), and foliation (layering of fabrics resulting from the alignment of min- eral grains or the development of compositional bands)
Contrast brittle and ductile deformation
brittle: cracking into pieces like a glass plate ductile: squeezing and becoming larger like dough under a book
What factors determine whether a rock will behave in brittle or ductile fashion?
- temperature - pressure - deformation rate -composition
How are stress and strain different?
stress- acting on a plane as the force applied per unit area of the plane strain- deformation in rock as result of stress
How is a fault different from a joint?
there is little to no lateral movement across joints. This makes joints different from a fault which is defined as a fracture in rock in which one side slides laterally past the other with a displacement that is greater than the separation between the blocks on either side of the fracture
How do you recognize faults in the field?
Faults may be recognized in the field three ways. (1) First as an abrupt change in elevation when the surrounding area is not similarly uplifted. (2) Second when there are dipping sediments that show an offset on either side of a line or trace of a presumed fault. (3) Third when there is a repeat of the sedimentary layers vertically. This last one is tricky as you need to know the expected sedimentary sequence for the area.
Describe the differences between an anticline, a syncline, and a monocline
anticlines: folds that shaped like an arch libs dip away from hinge synclines: limbs dip toward hinge monocline: resembles a carpet draped over a step ladder
Discuss the relationship between foliation and deformation
ductile deformation can cause tectonic foliation
Describe the principle of isostasy
the condition that exists when the buoyancy force pushing lithosphere up equals the gravitational force pulling lithosphere down
Deformation
Stress
Faults
Folding
craton
A long-lived block of durable continental crust commonly found in the stable interior of a continent.