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Geology 3120 Rock Fabric

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General definition - closely-spaced, aligned, planar to curviplanar penetrative surfaces ... What direction is the nearest anticline? Pressure Dissolution Cleavage ... – PowerPoint PPT presentation

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Title: Geology 3120 Rock Fabric


1
Geology 3120 - Rock Fabric
2
Objectives
  • Attitudes of Fabric
  • Cleavage
  • Lineations
  • Foliations

3
Fabrics
4
Fabrics
5
Fabrics
6
Fabrics
7
Cleavage
  • General definition - closely-spaced, aligned,
    planar to curviplanar penetrative surfaces
  • Continuous verses disjunctive cleavage - planar
    verses non-planar
  • Mechanical realignment and growth of clay
    minerals
  • Pressure dissolution process

8
Slaty Cleavage
  • Mechanical alignment and growth of clay minerals

9
Slaty Cleavage
  • Where is the bedding?

10
Slaty Cleavage
  • Where is the cleavage?

11
Slaty Cleavage
  • What direction is the nearest anticline?

12
Pressure Dissolution Cleavage
  • Extensional veins shortened in silt

13
Axial Planar Cleavage
  • Identify the folds

14
Axial Planar Cleavage
  • Identify the cleavage

15
Axial Planar Cleavage
  • Identify the axial surfaces

16
Axial Planar Cleavage
17
Axial Planar Cleavage
18
Bedding Axial Planar Cleavage Axial Surfaces
19
Cleavage Vergence
Central
East
West
20
Cleavage Vergence
West
Central
East
21
Cleavage Vergence
Central
West
East
22
Cleavage Vergence
Central
East
West
23
Pressure Solution Cleavage - Limestone
  • Insoluble material is typically contained in the
    stylolite

24
Introduction to Lineations
  • One-Dimensional Features
  • Slickenline lineations
  • Fault grooves
  • Stretched conglomerates
  • Boudins

25
Slickenline Lineations
  • Calcite mineral growth
  • on a fault plane

26
Grooves
  • Grooves are parallel to strike
  • What type of fault is this?

27
Stretched Conglomerates
Rock has a foliation, lineation depends on
whether clasts are disc- or rod-shaped
28
Boudins
29
Introduction to Foliations
  • Bring in the next dimension
  • Deformation or organization of grains with
    respect to a two-dimensional surface
  • Foliations in addition to lineations may yield
    information about the stretching direction

30
Foliations with Lineations
31
References
Slides 3 - 6 http//earth.leeds.ac.uk/minor/duc
tile/describing/lin-plane.htm Slide 1, 8 - 11
http//earth.leeds.ac.uk/minor/cleavage/slatey.htm
Slide 12 http//earth.leeds.ac.uk/minor/dmt/pso
lncleav.htm Slides 13 - 16 http//earth.leeds.ac
.uk/folds/describing/cleavage/cleavage.htm Slide
17 - 20 http//earth.leeds.ac.uk/folds/describin
g/cleavage/cleaverge.htm Slide 21
http//earth.leeds.ac.uk/minor/dmt/stilolite.htm S
lide 23 http//earth.leeds.ac.uk/minor/faults/str
ifibres.htm Slide 24 http//earth.leeds.ac.uk/min
or/faults/grooves.htm Slide 25
http//earth.leeds.ac.uk/minor/ductile/vasgo/congs
.htm Slide 26 http//earth.leeds.ac.uk/minor/ext
end/boudyke.htm Slide 26 http//earth.leeds.ac.u
k/strain/gallery/boudin.html Slide 28
http//earth.leeds.ac.uk/minor/ductile/vasgo/mylli
n.htm Slide 29 http//earth.leeds.ac.uk/minor/duc
tile/gallery/plattgen.htm
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