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Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS

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Page 1: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

Chapter 9 – FOLDS, FAULTS & GEOLOGIC

MAPS

Page 2: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

Rock Deformation• Stress

– Force acting on surface, per unit area

• Pressure– Confining (uniform)

• Stress is equal from all directions

– Differential stress• Stress is stronger from

some directions

• Strain– Change in rock shape or

volume in response to stress

Page 3: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Tension– Divergent boundaries– Normal faults

• Compression– Convergent

boundaries– Reverse faults

• Shear– Transform boundaries– Strike-slip faults

Rock Deformation

Page 4: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Elastic deformation– Temporary change;

rebounds when stress is gone

– Elastic limit (AKA yield point)

• Ductile deformation– Permanent, gradual

change; folds or bends– AKA Plastic deformation

• Brittle deformation– Permanent change;

breaks or cracks

Rock Deformation

Page 5: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Factors affecting rock deformation– Temperature– Confining pressure– Rate of deformation– Composition

• Structural geology – Study of stress & strain

• Strike– Compass orientation of line of

intersection between horizontal plane & planar feature

• Dip– Angle between tilted surface &

horizontal plane

Rock Deformation & Structural Geology

Page 6: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Faults & fractures: Dip-slip faults– Normal fault

• Hanging wall moves downward relative to footwall below

– Reverse fault• Hanging wall

moves up & over footwall below

– Thrust fault• Reverse fault with

shallow dip angle

Structural Geology

Page 7: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Strike-slip fault– Movement is horizontal &

parallel to strike of fault• Right-lateral• Left-lateral• San Andreas Fault

Structural Geology

Page 8: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Folds– Bend or warp in layered rock

• Monocline– 1-sided fold

• Anticline– Layers fold upward (arch)– Older rocks in core

• Syncline– Layers fold downward (trough)– Younger rocks in core

• Dome– Broad area of up-warping

• Basin– Broad area of down-warping

Structural Geology

Page 9: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

Geologic Maps• Geologic map

– Shows locations, kinds, & orientation of rock units

– Shows structural features • Topographic maps

– Shows shape of ground surface, as well as location & elevation of surface features

– Relief• Contour lines

• Geologic cross section– Diagram of geologic features

underground

Page 10: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

Chapter 10 –METAMORPHISM: NEW

ROCKS FROM OLD

Page 11: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

What is Metamorphism?• Metamorphism

– Mineralogical, textural, chemical & structural changes in rocks

– Rocks exposed to elevated temperatures &/or pressure• Rocks do NOT melt

Page 12: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Factors that influence metamorphism– Temperature

• 150°C = “official” boundary between diagenesis & metamorphism

– Pressure– Composition– Pore fluids

• Pores– Open spaces in rocks

• Migmatite– Transition between metamorphic &

igneous rocks

What is Metamorphism?

stress

stress

Page 13: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Factors that influence metamorphism (cont’d)– Stress

• Foliation– Planar arrangement of textural features in

metamorphic rock– Gives rock layered or banded appearance

– Duration– Rate of metamorphism

What is Metamorphism?

Page 14: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Grade– Degree of temperature & pressure a rock is exposed to during

metamorphism• Low-grade

– Low temperature & pressure conditions; minimal rock changes• High-grade

– High temperature & pressure conditions; significant rock changes

What is Metamorphism?

Page 15: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

Metamorphic Rocks

Texture Metamorphic Rock Parent Rock

Foliated

Slate Mudstone or shale

Phyllite Mudstone, shale or slateSchist Mudstone, shale, slate or phyllite

Gneiss Mudstone, shale, slate, phyllite, schist, granite, or diorite

Foliated or Nonfoliated

Amphibolite Basalt, gabbro or ultramafic igneous rocks

Nonfoliated

Anthracite Coal Peat, lignite, bituminous coal

Hornfels Any type of rock

Serpentinite Basalt, gabbro or ultramafic igneous rocks

Soapstone Basalt, gabbro or ultramafic igneous rocksQuartzite Sandstone

Marble Limestone

Metaconglomerate Conglomerate

• Texture: foliation• Composition: minerals present

Page 16: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

Metamorphic Rocks• Rocks with foliation

– Slate• Very fine grained metamorphic rock; low grade• Metamorphic product of shale

– Phyllite• Fine grained metamorphic rock; intermediate grade• Further metamorphism of slate

Page 17: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

Metamorphic Rocks• Rocks with foliation

– Schist• Visible individual mineral grains; intermediate grade• Further metamorphism of phyllite

– Gneiss• Course grained,

high grade, strongly foliated (light/dark bands)

• Further metamorphism of schist

Page 18: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Rocks without foliation– Quartzite

• Metamorphosed sandstone– Marble

• Metamorphosed limestone

Metamorphic Rocks

Page 19: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Type of metamorphism– Contact metamorphism

• Rocks heated & chemically changed adjacent to magma intrusion

• Aureole– Burial metamorphism

• Occurs after diagenesis• Due to burial of sediments in

deep sedimentary basins

Metamorphic Processes

Page 20: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

• Type of metamorphism – Regional metamorphism

• Metamorphism of extensive area of crust

• Plate convergence, collision, subduction

– Other types of metamorphism• Fault zone• Shock• Pyro-metamorphism

Metamorphic Processes

Page 21: Chapter 9 – FOLDS, FAULTS & GEOLOGIC MAPS. Rock Deformation Stress –Force acting on surface, per unit area Pressure –Confining (uniform) Stress is equal

Metamorphic Facies• Index minerals

– Minerals that form at specific temperature & pressure conditions

• Isograds– Lines of equal grade– Used to map index minerals