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Geology 3120 - Sedimentary Structures

Geology 3120 - Sedimentary Structures. Outline. Review the geologic history exercise from last time Contacts, primary structures, and secondary structures How to determine which “way is up”… Cross-bedding, graded-bedding, reverse graded-bedding

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Geology 3120 - Sedimentary Structures

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  1. Geology 3120 - Sedimentary Structures

  2. Outline • Review the geologic history exercise from last time • Contacts, primary structures, and secondary structures • How to determine which “way is up”… • Cross-bedding, graded-bedding, reverse graded-bedding • Determining way up using top surface features - ripples, mudcracks, raindrops, footprints • Determining way up using bottom surface features - load casts • Determining way up using features within rocks - geopetal, bioturbation, stromatolites, flame structures, pillow lavas

  3. Block model for exercise

  4. Geologic History • 12 Ma dike • 15 Ma dike • Normal fault • 20 Ma sed • 22 Ma sed • Erosion • Thrust fault • Folding • Layer B • 60 Ma sed • Layer G • 70 Ma sed • 80 Ma sed

  5. Contacts, Primary Structures & Secondary Structures • Contact - a boundary between rock units • Primary structure - structures that form during lithification • Secondary structure - structures that form after lithificaiton

  6. Contacts, Primary Structures & Secondary Structures • Contact - a boundary between rock units • Primary structure - structures that form during lithification • Secondary structure - structures that form after lithificaiton

  7. Which way is up? Today Option 1 Overturned syncline Option 2 “up side down” overturned anticline

  8. Cross-bedding Checkerboard Mesa, Zion National Park Younger Flow direction Y Concave up Older

  9. Graded bedding Younger Y Older • Decrease in depositional energy with sedimentation • Example: flood deposits, turbidity currents

  10. Graded bedding Younger Y Older • Decrease in depositional energy with sedimentation • Example: flood deposits, turbidity currents

  11. Reverse (Inverse) Graded Bedding Younger Y Older • Increase in depositional energy with sedimentation • Example: debris flows (a lot less common than normal graded beds)

  12. Ripple marks Y • Symmetric ripples indicate bi-modal current • Concave = up • Asymmetric ripples indicate unidirectional current

  13. Mud cracks • Desiccation of muddy sediments • Mud cracks 5 cm

  14. Raindrops Y • Limited to terrestrial sediments

  15. Footprints Y • Limited to terrestrial sediments

  16. Load casts • Protrusion of material into a layer below • Load casts indicate the base of a layer, not the top of a layer • Determining the current direction may be possible

  17. Geopetal Structures Y • A “natural” carpenter’s level Shell or cavity in the rock Matrix Infill material (I.e., calcite)

  18. Y Bioturbation • Habitation burrows • Feeding burrows • Movement

  19. Stromatolites Y • Sharks Bay, Australia • Cyanobacteria grow upward toward the surface

  20. Flame structures Y • Less dense material intrudes into material above • Caused by rapid loading of turbidite sands

  21. Pillow lava Y Upper curved surface “V “ notch

  22. References Slide 8 http://www.utahpictures.com/Checkerboard.html Slides 9-15, 17 Busch, R. M. and D. Tasa, Laboratory Manual in Physical Geology, 3rd. Ed., American Geological Institute and National Association of Geology Teachers, 260 p., 1990. Slide 18 http://www.discoverwest.com.au/hablin.html Slide 20 http://volcanoes.usgs.gov/Products/Pglossary/PillowLava.html http://volcanoes.usgs.gov/Products/Pglossary/ancientseq.html

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