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Geology 3120 - Kinematic Indicators in Shear Zones. Outline. What to look for Kinematic indicators. What to look for. Lines or Planes Rotation Mineral Growth Cross-Cutting Relationships. Offset and Deflected Markers. How would you describe the kinematics of this system?.
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Outline • What to look for • Kinematic indicators
What to look for • Lines or Planes • Rotation • Mineral Growth • Cross-Cutting Relationships
Offset and Deflected Markers How would you describe the kinematics of this system?
Offset and Deflected Markers Right-lateral offset
Foliation How would you describe the kinematics of this system?
Foliation Left-lateral offset
Foliations (S-C fabric) • Foliation develops as a result of simple shear • Dominant simple-shear parallel to walls of shear zone develops a S-surface foliation • New foliation develops (C-surface) at an angle (18-25 to the shear-zone walls)
S-C Fabric • S-surfaces - foliation planes • C-surfaces - shear bands (useful for determining the sense of shear)
S-C Fabric Right-lateral motion
Foliation (mica) fish • A layer with oblique internal fabric becomes detached along S-fabric to form an asymmetric ‘fish’. Fish “flash” - oriented sample reflected sunlight…
Mica Fish • If you can stack the fish up, you’ve got the sense of shear correct. Or, think of the fish as thrust surfaces…
Mica Fish Right-lateral movement
Porphyoblasts / Porphyroclasts • Porphyroblasts = large grains that have grown in the rock mass during deformation and metamorphism • Porphyroclasts = relict earlier large grains that have survived ductile deformation (e.g. feldspar) Blast: grain size increase Clast: grain size decrease
Tails on porphyroclasts are asymmetric in the direction of ductile flow.
Rotation ? ? • Works for inclusions, porphyroblasts, and porphyroclasts • Tails and fabric in the rotated grains are useful
Rotation CW • Right-lateral shear (dextral)
Mylonitic orthogneiss - Nash Fork Shear Zone, Medicine Bow Mtns, So. Wyoming. K-spar porphyroclasts with asymmetric tails What is sense of shear here?
Pressure Shadows with Fiber Growth • Minerals will grow in the direction of maximum extension
Pressure Shadows with Fiber Growth Maximum extension Maximum shortening
Fractured Grains How would you describe the kinematics of this system?
Fractured Grains • Large grains of some minerals (e.g. feldspars, pyroxenes) continue to deform brittley within a ductile matrix. • The fractures indicate a sense of motion opposite that of actual shear sense How would you describe the kinematics of this system?
Fractured Grains Right-lateral offset
Veins • Calcite extensional vein
Tension Gashes • Initial shearing
Tension Gashes • Directions of maximum extension and maximum shortening
Tension Gashes • Mode I (opening) fracture develops
Tension Gashes • Continued development of a tension gash
Tension Gashes How would you describe the kinematics of this system?
Tension Gashes Finally, left-lateral motion!!!
Tension Gashes How would you describe the kinematics of this system?
Tension Gashes Left-lateral motion
References Slide 1: http://earth.leeds.ac.uk/shearzones/gallery/odhair.htm Slides 4, 5: http://earth.leeds.ac.uk/shearzones/gallery/apliteshear.htm Slides 6, 7:http://earth.leeds.ac.uk/shearzones/gallery/kohi1.htm Slides 8, 9: http://www.earth.monash.edu.au/Teaching/mscourse/lectures/lec4b.html Slides 10,11: Image 30 at http://talc.geo.umn.edu/orgs/struct/microstructure/sec2.html Slides 12, 13:http://www.uni-mainz.de/~mezger/Text/Mezger_metamorphic_geology.html Slides 14, 15:http://earth.leeds.ac.uk/strain/gallery/presshadbig.html Slides 16, 17:http://www.earth.monash.edu.au/Teaching/mscourse/lectures/lec4b.html Slide 18:http://earth.leeds.ac.uk/minor/dmt/reprecipitation.htm Slides 19 - 22:http://earth.leeds.ac.uk/minor/tensiongash/gash1.htm Slides 23 - 24:http://earth.leeds.ac.uk/minor/tensiongash/tgash.htm Slide 25:http://earth.leeds.ac.uk/minor/tensiongash/gash3.htm Slides 26 - 27: http://earth.leeds.ac.uk/minor/tensiongash/gashpic2.htm