geology 3120 - rock fabric

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Geology 3120 - Rock Fabric Geology 3120 - Rock Fabric

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Geology 3120 - Rock Fabric. Objectives. Attitudes of Fabric Cleavage Lineations Foliations. Fabrics. Fabrics. Fabrics. Fabrics. Cleavage. General definition - closely-spaced, aligned, planar to curviplanar penetrative surfaces - PowerPoint PPT Presentation

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Page 1: Geology 3120 - Rock Fabric

Geology 3120 - Rock FabricGeology 3120 - Rock Fabric

Page 2: Geology 3120 - Rock Fabric

ObjectivesObjectives

• Attitudes of FabricAttitudes of Fabric• CleavageCleavage• LineationsLineations• FoliationsFoliations

Page 3: Geology 3120 - Rock Fabric

FabricsFabrics

Page 4: Geology 3120 - Rock Fabric

FabricsFabrics

Page 5: Geology 3120 - Rock Fabric

FabricsFabrics

Page 6: Geology 3120 - Rock Fabric

FabricsFabrics

Page 7: Geology 3120 - Rock Fabric

CleavageCleavage

• General definition - closely-spaced, aligned, planar to General definition - closely-spaced, aligned, planar to

curviplanar penetrative surfacescurviplanar penetrative surfaces

• ContinuousContinuous verses verses disjunctivedisjunctive cleavage - planar verses cleavage - planar verses

non-planarnon-planar

• Mechanical realignment and growth of clay mineralsMechanical realignment and growth of clay minerals

• Pressure dissolution processPressure dissolution process

Page 8: Geology 3120 - Rock Fabric

Slaty CleavageSlaty Cleavage

Mechanical alignment and growth of clay mineralsMechanical alignment and growth of clay minerals

Page 9: Geology 3120 - Rock Fabric

Slaty CleavageSlaty Cleavage

Where is the bedding?Where is the bedding?

Page 10: Geology 3120 - Rock Fabric

Slaty CleavageSlaty Cleavage

Where is the cleavage?Where is the cleavage?

Page 11: Geology 3120 - Rock Fabric

Slaty CleavageSlaty Cleavage

What direction is the nearest anticline?What direction is the nearest anticline?

Page 12: Geology 3120 - Rock Fabric

Pressure Dissolution CleavagePressure Dissolution Cleavage

Extensional veins shortened in silt

Page 13: Geology 3120 - Rock Fabric

Axial Planar CleavageAxial Planar Cleavage

Identify the folds

Page 14: Geology 3120 - Rock Fabric

Axial Planar CleavageAxial Planar Cleavage

Identify the cleavage

Page 15: Geology 3120 - Rock Fabric

Axial Planar CleavageAxial Planar Cleavage

Identify the axial surfaces

Page 16: Geology 3120 - Rock Fabric

Axial Planar CleavageAxial Planar Cleavage

Page 17: Geology 3120 - Rock Fabric

Axial Planar CleavageAxial Planar Cleavage

Page 18: Geology 3120 - Rock Fabric

BeddingBedding

Axial Planar CleavageAxial Planar Cleavage

Axial SurfacesAxial Surfaces

Page 19: Geology 3120 - Rock Fabric

Cleavage VergenceCleavage Vergence

WestCentral East

Page 20: Geology 3120 - Rock Fabric

Cleavage VergenceCleavage Vergence

West Central East

Page 21: Geology 3120 - Rock Fabric

Cleavage VergenceCleavage Vergence

WestCentralCentral

East

Page 22: Geology 3120 - Rock Fabric

Cleavage VergenceCleavage Vergence

WestCentralCentral

East

Page 23: Geology 3120 - Rock Fabric

Pressure Solution Cleavage - Pressure Solution Cleavage - LimestoneLimestone

Insoluble material is typically contained in the stylolite

Page 24: Geology 3120 - Rock Fabric

Introduction to LineationsIntroduction to Lineations

One-Dimensional Features One-Dimensional Features

Slickenline lineationsSlickenline lineations

Fault groovesFault grooves

Stretched conglomeratesStretched conglomerates

BoudinsBoudins

Page 25: Geology 3120 - Rock Fabric

Slickenline LineationsSlickenline Lineations

Calcite mineral growth

on a fault plane

Page 26: Geology 3120 - Rock Fabric

GroovesGrooves

Grooves are parallel to strikeGrooves are parallel to strike

What type of fault is this?What type of fault is this?

Page 27: Geology 3120 - Rock Fabric

Stretched ConglomeratesStretched Conglomerates

Rock has a foliation, lineation depends on whether clasts areRock has a foliation, lineation depends on whether clasts are

disc- or rod-shapeddisc- or rod-shaped

Page 28: Geology 3120 - Rock Fabric

Boudins Boudins

Page 29: Geology 3120 - Rock Fabric

Introduction to FoliationsIntroduction to Foliations

Bring in the next dimensionBring in the next dimension

Deformation or organization of grains with respect to Deformation or organization of grains with respect to

a two-dimensional surfacea two-dimensional surface

Foliations in addition to lineations may yield Foliations in addition to lineations may yield

information about the stretching direction information about the stretching direction

Page 30: Geology 3120 - Rock Fabric

Foliations with LineationsFoliations with Lineations

Page 31: Geology 3120 - Rock Fabric

ReferencesReferencesSlides 3 - 6: Slides 3 - 6: http://earth.leeds.ac.uk/minor/ductile/describing/lin-plane.htm

Slide 1, 8 - 11: Slide 1, 8 - 11: http://earth.leeds.ac.uk/minor/cleavage/slatey.htm

Slide 12Slide 12: : http://earth.leeds.ac.uk/minor/dmt/psolncleav.htm

Slides 13 - 16: Slides 13 - 16: http://earth.leeds.ac.uk/folds/describing/cleavage/cleavage.htm

Slide 17 - 20Slide 17 - 20: http://earth.leeds.ac.uk/folds/describing/cleavage/cleaverge.htm: http://earth.leeds.ac.uk/folds/describing/cleavage/cleaverge.htm

Slide 21Slide 21: http://earth.leeds.ac.uk/minor/dmt/stilolite.htm: http://earth.leeds.ac.uk/minor/dmt/stilolite.htm

Slide 23Slide 23: http://earth.leeds.ac.uk/minor/faults/strifibres.htm: http://earth.leeds.ac.uk/minor/faults/strifibres.htm

Slide 24Slide 24: http://earth.leeds.ac.uk/minor/faults/grooves.htm: http://earth.leeds.ac.uk/minor/faults/grooves.htm

Slide 25Slide 25: http://earth.leeds.ac.uk/minor/ductile/vasgo/congs.htm: http://earth.leeds.ac.uk/minor/ductile/vasgo/congs.htm

Slide 26Slide 26: http://earth.leeds.ac.uk/minor/extend/boudyke.htm: http://earth.leeds.ac.uk/minor/extend/boudyke.htm

Slide 26Slide 26: http://earth.leeds.ac.uk/strain/gallery/boudin.html: http://earth.leeds.ac.uk/strain/gallery/boudin.html

Slide 28:Slide 28: http://earth.leeds.ac.uk/minor/ductile/vasgo/myllin.htm http://earth.leeds.ac.uk/minor/ductile/vasgo/myllin.htm

Slide 29:Slide 29: http://earth.leeds.ac.uk/minor/ductile/gallery/plattgen.htm http://earth.leeds.ac.uk/minor/ductile/gallery/plattgen.htm