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Folds, Faults and Other Records of Deformation. Significance to CCS. Fundamental to trapping configuration Important for caprock integrity. Stress. Force per unit area Compression Tension (rare) Shearing. Or, principal compressive stress vertical. Brittle Versus Ductile Deformation.
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Significance to CCS • Fundamental to trapping configuration • Important for caprock integrity
Stress • Force per unit area • Compression • Tension (rare) • Shearing
Or, principal compressive stress vertical
Brittle Versus Ductile Deformation • Brittle: material fractures (breaks)
Brittle Versus Ductile Deformation • Brittle: material fractures (breaks) • Ductile: plastic deformation, no fractures
Brittle Versus Ductile Deformation • Brittle: material fractures (breaks) • Ductile: plastic deformation, no fractures • Brittle favored by:
Brittle Versus Ductile Deformation • Brittle: material fractures (breaks) • Ductile: plastic deformation, no fractures • Brittle favored by: • low temperatures
Brittle Versus Ductile Deformation • Brittle: material fractures (breaks) • Ductile: plastic deformation, no fractures • Brittle favored by: • low temperatures • low confining pressures
High confining pressure Low confining pressure Undeformed
Brittle Versus Ductile Deformation • Brittle: material fractures (breaks) • Ductile: plastic deformation, no fractures • Brittle favored by: • low temperatures • low confining pressures • high strain rates • Rock type
Mapping Geologic Structures Strike Dip
Mapping Geologic Structures • Strike • Dip • Constructing cross sections
Folds Bending of rocks, often as a result of compression
Symmetrical, Asymmetrical, Overturned Limbs of equal length Limbs of unequal length
Faults and Joints Fractures in rock
Joints • No visible displacement • Types • Unloading (exfoliation)
Joints • No visible displacement • Types • Unloading (exfoliation) • Cooling joints