1 / 32

Lab 7 – Structural Geology Chapter 10

Lab 7 – Structural Geology Chapter 10. Turn In: Lab 6 Pre-Lab 7 EC 2 Handouts: Quiz 6 Lab 7 Pre-Lab 8. Deformation. STRESS - direct pressure on the rock. Compressive = shorten Tensional = extension STRAIN – when rock is stressed to the point of failure = permanent deformation.

rafi
Download Presentation

Lab 7 – Structural Geology Chapter 10

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Lab 7 – Structural GeologyChapter 10 Turn In: Lab 6 Pre-Lab 7 EC 2 Handouts: Quiz 6 Lab 7 Pre-Lab 8

  2. Deformation • STRESS - direct pressure on the rock. • Compressive = shorten • Tensional = extension • STRAIN – when rock is stressed to the point of failure = permanent deformation. http://www.tulane.edu/~sanelson/images/deformmeta.gif

  3. Bedsare said to be dipping if they are oriented more than 0o from horizontal. (A cross-section sort of thing.)Dip direction is the compass direction a marble would roll down the top of the individual bed. (Not the topography…)(A map view sort of thing.)Which compass direction do these beds appear to be dipping? (view looking approximately south) W

  4. Dip angleis the angle between horizontal and the flat face of the bed. (A cross-section sort of thing.)How much do these beds appear to be dipping? (view looking approximately south) ~35o W

  5. Strikeis the compass direction 90o from the dip direction, and is one direction in which beds are laterally continuous.(A map view sort of thing.)Approximately which compass direction do these beds appear to be striking? (view looking approximately south) ~35o W

  6. What does this look like in map view? 20 20 20 20 A A’ * * Topo map review – find the valley and the ridges Geol map stuff – find the strike and dip symbols What are the map units relative to the picture? TS2 TB1 Tertiary seds Tertiary basalt 1 TB2 Tertiary basalt 2 (view looking southwest) N

  7. What does this look like in cross-section? A A’ 20 20 20 20 A A’ * * Sketch only – NOT TO SCALE. TS2 TB1 Tertiary seds Tertiary basalt 1 TB2 Tertiary basalt 2 (view looking southwest) N

  8. Quick Review: Identify the approximate dip direction, dip angle, and strike in the close outcrop. ~??o

  9. The name of a landform is determined by how the beds dip…A side effect is the relations of older and younger beds…

  10. Folds and Block Diagrams • Anticline = oldest rocks exposed in the center. • Syncline = youngest rocks exposed in the center

  11. Which directions are these beds dipping?What are the relations of older and younger beds?What are the names of the landforms?

  12. Which way are the beds dipping? What are the landforms? www.geology.wisc.edu/courses/g112 CFW ‘07

  13. Which feature has on overturned limb? Which way is up on each limb? web.uct.ac.za/depts/geolsci/dlr/laingsburg www.geology.wisc.edu/courses/g112

  14. Economic Look • Folds in alternating permeable and impermeable layers = traps. • Can trap water, oil, etc… http://www.emporia.edu/earthsci/amber/students/shirley/anticlinetrap.gif

  15. http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php Mt. Withrow As the Rocky Mountains formed, the strata (rock layers) of the Earth's crust were subjected to stress which resulted in strain (folding). Ridges = resistant sandstone Valley = much less resistant shale. Which way are the beds dipping? Where is the nose? What is the name of the structure? Which way is it plunging?

  16. Stress Types and Faults • Compressive Stress:causes shortening of the body on which it acts • Reverse or Thrust Fault: one rock gets pushed up over another.

  17. Stress Types and Faults • Tensional Stress: Causes lengthening of the body on which it acts • Normal Fault: One rock slides down and away from another

  18. Stress Types and Faults • Shear Stress:Causes shearing/tearing of the body on which it acts. • Strike-Slip Fault: One rock slides past another horizontally.

  19. Quick Review of Map Views – In each picture: Which units are oldest/youngest? Which way are the beds dipping? What structures are present?

  20. Seismic Interpretation • Offshore Netherlands “F3” dataset courtesy of Paul deGroot of dGB • Open-source seismic software from OpendTect.org

  21. Seismic Interpretation Lab • 1) Strike and Dip • Put at least 10 strike-and-dip symbols on the horizontal section, consulting the vertical section as needed. • Identify and label a dome. • Identify and label a basin. • For the dome and basin you interpreted, explain the observations that support your interpretations. Point out the observations noted on your sections: • Offshore Netherlands “F3” dataset courtesy of Paul deGroot of dGB • Open-source seismic software from OpendTect.org

  22. Seismic Interpretation Lab Ex. 1 horizontal section

  23. Seismic Interpretation Lab Ex. 1 vertical section

  24. 2) Plunging Fold • On the east side of the horizontal section is a plunging fold. Mark some strikes and dips around it, referring to the vertical sections. • Interpret whether the fold is an anticline or syncline: • Interpret which direction the fold is plunging: • Label the fold on the horizontal section with the proper symbol at its axis. • Describe how your observations support your interpretations:

  25. Seismic Interpretation Lab Ex. 2, 3 horizontal section

  26. Seismic Interpretation Lab Ex. 2-5 vertical section Inline 102

  27. Seismic Interpretation Lab Ex. 2-5 vertical section Inline 190

  28. Seismic Interpretation Lab Ex. 2-5 vertical section Inline 290

  29. Seismic Interpretation Lab Ex. 2-5 vertical section Inline 390

  30. Seismic Interpretation Lab Ex. 2-5 vertical section Inline 490

  31. 3) Fault Tracing • On the east side of the horizontal section is a prominent fault. Mark the fault on the horizontal section. • Mark the same fault on each of the vertical sections, if it appears on that section. • What is the average strike direction of the fault? Average dip and direction? • What is the sense of offset on the fault: horizontal; or vertical? • What type of fault is it: reverse; thrust; normal; or strike-slip? • Complete the labeling of the fault on the horizontal section with the proper symbol. • Mark where the fault terminates on the horizontal section. • Discuss whether you can rule out that this fault has oblique slip. Could it be a mixture of types?

  32. 4) Unconformities • On the east side near the middle of each vertical section there are several unconformities (originating in a hiatus of sedimentation between deposition of delta lobes). These are evident as terminations of one bed (reflection) against another. Go through the 5 vertical sections and mark at least 5 terminations on each, with a short arrow pointing along a bed to its termination. • Mark one unconformity across all 5 vertical sections with the wiggly line symbol. • 5) Reservoirs • Reservoirs of fluid (oil, gas, water, steam) trapped in the rock pore spaces tend to make seismic bright spots. Circle a few bright spots on the Inline vertical sections 102 and 190. • Discuss whether these potential oil reservoirs may be associated with any of the other features you have interpreted.

More Related